Articles | Volume 4, issue 2
https://doi.org/10.5194/se-4-277-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-4-277-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Extreme extension across Seram and Ambon, eastern Indonesia: evidence for Banda slab rollback
J. M. Pownall
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham TW20 0EX, UK
R. Hall
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham TW20 0EX, UK
I. M. Watkinson
SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham TW20 0EX, UK
Related subject area
Tectonics
Analogue modelling of basin inversion: a review and future perspectives
Insights into the interaction of a shale with CO2
Tectonostratigraphic evolution of the Slyne Basin
Assessing the role of thermal disequilibrium in the evolution of the lithosphere–asthenosphere boundary: an idealized model of heat exchange during channelized melt transport
Control of crustal strength, tectonic inheritance, and stretching/ shortening rates on crustal deformation and basin reactivation: insights from laboratory models
Numerical simulation of contemporary kinematics at the northeastern Tibetan Plateau and its implications for seismic hazard assessment
Construction of the Ukrainian Carpathian Wedge from low-temperature thermochronology and tectono-stratigraphic analysis
Late Cretaceous–early Palaeogene inversion-related tectonic structures at the northeastern margin of the Bohemian Massif (southwestern Poland and northern Czechia)
A tectonic-rules-based mantle reference frame since 1 billion years ago – implications for supercontinent cycles and plate–mantle system evolution
An efficient partial-differential-equation-based method to compute pressure boundary conditions in regional geodynamic models
The analysis of slip tendency of major tectonic faults in Germany
Earthquake ruptures and topography of the Chilean margin controlled by plate interface deformation
Together but separate: decoupled Variscan (late Carboniferous) and Alpine (Late Cretaceous–Paleogene) inversion tectonics in NW Poland
Late Quaternary faulting in the southern Matese (Italy): implications for earthquake potential and slip rate variability in the southern Apennines
The topographic signature of temperature-controlled rheological transitions in an accretionary prism
Rare earth elements associated with carbonatite–alkaline complexes in western Rajasthan, India: exploration targeting at regional scale
Exhumation and erosion of the Northern Apennines, Italy: new insights from low-temperature thermochronometers
Structural complexities and tectonic barriers controlling recent seismic activity in the Pollino area (Calabria–Lucania, southern Italy) – constraints from stress inversion and 3D fault model building
The Mid Atlantic Appalachian Orogen Traverse: a comparison of virtual and on-location field-based capstone experiences
Chronology of thrust propagation from an updated tectono-sedimentary framework of the Miocene molasse (western Alps)
Orogenic lithosphere and slabs in the greater Alpine area – interpretations based on teleseismic P-wave tomography
Ground-penetrating radar signature of Quaternary faulting: a study from the Mt. Pollino region, southern Apennines, Italy
U–Pb dating of middle Eocene–Pliocene multiple tectonic pulses in the Alpine foreland
Detrital zircon provenance record of the Zagros mountain building from the Neotethys obduction to the Arabia–Eurasia collision, NW Zagros fold–thrust belt, Kurdistan region of Iraq
The Subhercynian Basin: an example of an intraplate foreland basin due to a broken plate
Late to post-Variscan basement segmentation and differential exhumation along the SW Bohemian Massif, central Europe
Holocene surface-rupturing earthquakes on the Dinaric Fault System, western Slovenia
Contribution of gravity gliding in salt-bearing rift basins – a new experimental setup for simulating salt tectonics under the influence of sub-salt extension and tilting
3D crustal stress state of Germany according to a data-calibrated geomechanical model
Thick- and thin-skinned basin inversion in the Danish Central Graben, North Sea – the role of deep evaporites and basement kinematics
Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models
Interactions of plutons and detachments: a comparison of Aegean and Tyrrhenian granitoids
Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece
Stress rotation – impact and interaction of rock stiffness and faults
Looking beyond kinematics: 3D thermo-mechanical modelling reveals the dynamics of transform margins
Conditional probability of distributed surface rupturing during normal-faulting earthquakes
Late Cretaceous to Paleogene exhumation in central Europe – localized inversion vs. large-scale domal uplift
Kinematics and extent of the Piemont–Liguria Basin – implications for subduction processes in the Alps
Contrasting exhumation histories and relief development within the Three Rivers Region (south-east Tibet)
A systems-based approach to parameterise seismic hazard in regions with little historical or instrumental seismicity: active fault and seismogenic source databases for southern Malawi
Effects of basal drag on subduction dynamics from 2D numerical models
Hydrocarbon accumulation in basins with multiple phases of extension and inversion: examples from the Western Desert (Egypt) and the western Black Sea
Long-wavelength late-Miocene thrusting in the north Alpine foreland: implications for late orogenic processes
Characteristics of earthquake ruptures and dynamic off-fault deformation on propagating faults
A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The enigmatic curvature of Central Iberia and its puzzling kinematics
Control of 3-D tectonic inheritance on fold-and-thrust belts: insights from 3-D numerical models and application to the Helvetic nappe system
Plio-Quaternary tectonic evolution of the southern margin of the Alboran Basin (Western Mediterranean)
Surface deformation relating to the 2018 Lake Muir earthquake sequence, southwest Western Australia: new insight into stable continental region earthquakes
Seismic reflection data reveal the 3D structure of the newly discovered Exmouth Dyke Swarm, offshore NW Australia
Frank Zwaan, Guido Schreurs, Susanne J. H. Buiter, Oriol Ferrer, Riccardo Reitano, Michael Rudolf, and Ernst Willingshofer
Solid Earth, 13, 1859–1905, https://doi.org/10.5194/se-13-1859-2022, https://doi.org/10.5194/se-13-1859-2022, 2022
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When a sedimentary basin is subjected to compressional tectonic forces after its formation, it may be inverted. A thorough understanding of such
basin inversionis of great importance for scientific, societal, and economic reasons, and analogue tectonic models form a key part of our efforts to study these processes. We review the advances in the field of basin inversion modelling, showing how the modelling results can be applied, and we identify promising venues for future research.
Eleni Stavropoulou and Lyesse Laloui
Solid Earth, 13, 1823–1841, https://doi.org/10.5194/se-13-1823-2022, https://doi.org/10.5194/se-13-1823-2022, 2022
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Shales are identified as suitable caprock formations for geolocigal CO2 storage thanks to their low permeability. Here, small-sized shale samples are studied under field-representative conditions with X-ray tomography. The geochemical impact of CO2 on calcite-rich zones is for the first time visualised, the role of pre-existing micro-fissures in the CO2 invasion trapping in the matererial is highlighted, and the initiation of micro-cracks when in contact with anhydrous CO2 is demonstrated.
Conor M. O'Sullivan, Conrad J. Childs, Muhammad M. Saqab, John J. Walsh, and Patrick M. Shannon
Solid Earth, 13, 1649–1671, https://doi.org/10.5194/se-13-1649-2022, https://doi.org/10.5194/se-13-1649-2022, 2022
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The Slyne Basin is a sedimentary basin located offshore north-western Ireland. It formed through a long and complex evolution involving distinct periods of extension. The basin is subdivided into smaller basins, separated by deep structures related to the ancient Caledonian mountain-building event. These deep structures influence the shape of the basin as it evolves in a relatively unique way, where early faults follow these deep structures, but later faults do not.
Mousumi Roy
Solid Earth, 13, 1415–1430, https://doi.org/10.5194/se-13-1415-2022, https://doi.org/10.5194/se-13-1415-2022, 2022
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This study investigates one of the key processes that may lead to the destruction and destabilization of continental tectonic plates: the infiltration of buoyant, hot, molten rock (magma) into the base of the plate. Using simple calculations, I suggest that heating during melt–rock interaction may thermally perturb the tectonic plate, weakening it and potentially allowing it to be reshaped from beneath. Geochemical, petrologic, and geologic observations are used to guide model parameters.
Benjamin Guillaume, Guido M. Gianni, Jean-Jacques Kermarrec, and Khaled Bock
Solid Earth, 13, 1393–1414, https://doi.org/10.5194/se-13-1393-2022, https://doi.org/10.5194/se-13-1393-2022, 2022
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Under tectonic forces, the upper part of the crust can break along different types of faults, depending on the orientation of the applied stresses. Using scaled analogue models, we show that the relative magnitude of compressional and extensional forces as well as the presence of inherited structures resulting from previous stages of deformation control the location and type of faults. Our results gives insights into the tectonic evolution of areas showing complex patterns of deformation.
Liming Li, Xianrui Li, Fanyan Yang, Lili Pan, and Jingxiong Tian
Solid Earth, 13, 1371–1391, https://doi.org/10.5194/se-13-1371-2022, https://doi.org/10.5194/se-13-1371-2022, 2022
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We constructed a three-dimensional numerical geomechanics model to obtain the continuous slip rates of active faults and crustal velocities in the northeastern Tibetan Plateau. Based on the analysis of the fault kinematics in the study area, we evaluated the possibility of earthquakes occurring in the main faults in the area, and analyzed the crustal deformation mechanism of the northeastern Tibetan Plateau.
Marion Roger, Arjan de Leeuw, Peter van der Beek, Laurent Husson, Edward R. Sobel, Johannes Glodny, and Matthias Bernet
EGUsphere, https://doi.org/10.5194/egusphere-2022-828, https://doi.org/10.5194/egusphere-2022-828, 2022
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We study the construction of the Ukrainian Carpathians with LT thermochronology (AFT, AHe and ZHe) and stratigraphic analysis. QTQt thermal models are combined with burial diagrams to retrieve the timing and magnitude of sedimentary burial, tectonic burial and subsequent exhumation of the wedge’s nappes, from 34 to ~12 Ma. Out-of-sequence thrusting and sediment recycling during wedge building are also identified. This elucidates the evolution of a typical wedge in a roll-back subduction zone.
Andrzej Głuszyński and Paweł Aleksandrowski
Solid Earth, 13, 1219–1242, https://doi.org/10.5194/se-13-1219-2022, https://doi.org/10.5194/se-13-1219-2022, 2022
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Old seismic data recently reprocessed with modern software allowed us to study at depth the Late Cretaceous tectonic structures in the Permo-Mesozoic rock sequences in the Sudetes. The structures formed in response to Iberia collision with continental Europe. The NE–SW compression undulated the crystalline basement top and produced folds, faults and joints in the sedimentary cover. Our results are of importance for regional geology and in prospecting for deep thermal waters.
R. Dietmar Müller, Nicolas Flament, John Cannon, Michael G. Tetley, Simon E. Williams, Xianzhi Cao, Ömer F. Bodur, Sabin Zahirovic, and Andrew Merdith
Solid Earth, 13, 1127–1159, https://doi.org/10.5194/se-13-1127-2022, https://doi.org/10.5194/se-13-1127-2022, 2022
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We have built a community model for the evolution of the Earth's plate–mantle system. Created with open-source software and an open-access plate model, it covers the last billion years, including the formation, breakup, and dispersal of two supercontinents, as well as the creation and destruction of numerous ocean basins. The model allows us to
seeinto the Earth in 4D and helps us unravel the connections between surface tectonics and the
beating heartof the Earth, its convecting mantle.
Anthony Jourdon and Dave A. May
Solid Earth, 13, 1107–1125, https://doi.org/10.5194/se-13-1107-2022, https://doi.org/10.5194/se-13-1107-2022, 2022
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In this study we present a method to compute a reference pressure based on density structure in which we cast the problem in terms of a partial differential equation (PDE). We show in the context of 3D models of continental rifting that using the pressure as a boundary condition within the flow problem results in non-cylindrical velocity fields, producing strain localization in the lithosphere along large-scale strike-slip shear zones and allowing the formation and evolution of triple junctions.
Luisa Röckel, Steffen Ahlers, Birgit Müller, Karsten Reiter, Oliver Heidbach, Andreas Henk, Tobias Hergert, and Frank Schilling
Solid Earth, 13, 1087–1105, https://doi.org/10.5194/se-13-1087-2022, https://doi.org/10.5194/se-13-1087-2022, 2022
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Reactivation of tectonic faults can lead to earthquakes and jeopardize underground operations. The reactivation potential is linked to fault properties and the tectonic stress field. We create 3D geometries for major faults in Germany and use stress data from a 3D geomechanical–numerical model to calculate their reactivation potential and compare it to seismic events. The reactivation potential in general is highest for NNE–SSW- and NW–SE-striking faults and strongly depends on the fault dip.
Nadaya Cubas, Philippe Agard, and Roxane Tissandier
Solid Earth, 13, 779–792, https://doi.org/10.5194/se-13-779-2022, https://doi.org/10.5194/se-13-779-2022, 2022
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Earthquake extent prediction is limited by our poor understanding of slip deficit patterns. From a mechanical analysis applied along the Chilean margin, we show that earthquakes are bounded by extensive plate interface deformation. This deformation promotes stress build-up, leading to earthquake nucleation; earthquakes then propagate along smoothed fault planes and are stopped by heterogeneously distributed deformation. Slip deficit patterns reflect the spatial distribution of this deformation.
Piotr Krzywiec, Mateusz Kufrasa, Paweł Poprawa, Stanisław Mazur, Małgorzata Koperska, and Piotr Ślemp
Solid Earth, 13, 639–658, https://doi.org/10.5194/se-13-639-2022, https://doi.org/10.5194/se-13-639-2022, 2022
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Legacy 2-D seismic data with newly acquired 3-D seismic data were used to construct a new model of geological evolution of NW Poland over last 400 Myr. It illustrates how the destruction of the Caledonian orogen in the Late Devonian–early Carboniferous led to half-graben formation, how they were inverted in the late Carboniferous, how the study area evolved during the formation of the Permo-Mesozoic Polish Basin and how supra-evaporitic structures were inverted in the Late Cretaceous–Paleogene.
Paolo Boncio, Eugenio Auciello, Vincenzo Amato, Pietro Aucelli, Paola Petrosino, Anna C. Tangari, and Brian R. Jicha
Solid Earth, 13, 553–582, https://doi.org/10.5194/se-13-553-2022, https://doi.org/10.5194/se-13-553-2022, 2022
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We studied the Gioia Sannitica normal fault (GF) within the southern Matese fault system (SMF) in southern Apennines (Italy). It is a fault with a long slip history that has experienced recent reactivation or acceleration. Present activity has resulted in late Quaternary fault scarps and Holocene surface faulting. The maximum slip rate is ~ 0.5 mm/yr. Activation of the 11.5 km GF or the entire 30 km SMF can produce up to M 6.2 or M 6.8 earthquakes, respectively.
Sepideh Pajang, Laetitia Le Pourhiet, and Nadaya Cubas
Solid Earth, 13, 535–551, https://doi.org/10.5194/se-13-535-2022, https://doi.org/10.5194/se-13-535-2022, 2022
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The local topographic slope of an accretionary prism is often used to determine the effective friction on subduction megathrust. We investigate how the brittle–ductile and the smectite–illite transitions affect the topographic slope of an accretionary prism and its internal deformation to provide clues to determine the origin of observed low topographic slopes in subduction zones. We finally discuss their implications in terms of the forearc basin and forearc high genesis and nature.
Malcolm Aranha, Alok Porwal, Manikandan Sundaralingam, Ignacio González-Álvarez, Amber Markan, and Karunakar Rao
Solid Earth, 13, 497–518, https://doi.org/10.5194/se-13-497-2022, https://doi.org/10.5194/se-13-497-2022, 2022
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Rare earth elements (REEs) are considered critical mineral resources for future industrial growth due to their short supply and rising demand. This study applied an artificial-intelligence-based technique to target potential REE-deposit hosting areas in western Rajasthan, India. Uncertainties associated with the prospective targets were also estimated to aid decision-making. The presented workflow can be applied to similar regions elsewhere to locate potential zones of REE mineralisation.
Erica D. Erlanger, Maria Giuditta Fellin, and Sean D. Willett
Solid Earth, 13, 347–365, https://doi.org/10.5194/se-13-347-2022, https://doi.org/10.5194/se-13-347-2022, 2022
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We present an erosion rate analysis on dated rock and sediment from the Northern Apennine Mountains, Italy, which provides new insights on the pattern of erosion rates through space and time. This analysis shows decreasing erosion through time on the Ligurian side but increasing erosion through time on the Adriatic side. We suggest that the pattern of erosion rates is consistent with the present asymmetric topography in the Northern Apennines, which has likely existed for several million years.
Daniele Cirillo, Cristina Totaro, Giusy Lavecchia, Barbara Orecchio, Rita de Nardis, Debora Presti, Federica Ferrarini, Simone Bello, and Francesco Brozzetti
Solid Earth, 13, 205–228, https://doi.org/10.5194/se-13-205-2022, https://doi.org/10.5194/se-13-205-2022, 2022
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The Pollino region is a highly seismic area of Italy. Increasing the geological knowledge on areas like this contributes to reducing risk and saving lives. We reconstruct the 3D model of the faults which generated the 2010–2014 seismicity integrating geological and seismological data. Appropriate relationships based on the dimensions of the activated faults suggest that they did not fully discharge their seismic potential and could release further significant earthquakes in the near future.
Steven Whitmeyer, Lynn Fichter, Anita Marshall, and Hannah Liddle
Solid Earth, 12, 2803–2820, https://doi.org/10.5194/se-12-2803-2021, https://doi.org/10.5194/se-12-2803-2021, 2021
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Field trips in the Stratigraphy, Structure, Tectonics (SST) course transitioned to a virtual format in Fall 2020, due to the COVID pandemic. Virtual field experiences (VFEs) were developed in web Google Earth and were evaluated in comparison with on-location field trips via an online survey. Students recognized the value of VFEs for revisiting outcrops and noted improved accessibility for students with disabilities. Potential benefits of hybrid field experiences were also indicated.
Amir Kalifi, Philippe Hervé Leloup, Philippe Sorrel, Albert Galy, François Demory, Vincenzo Spina, Bastien Huet, Frédéric Quillévéré, Frédéric Ricciardi, Daniel Michoux, Kilian Lecacheur, Romain Grime, Bernard Pittet, and Jean-Loup Rubino
Solid Earth, 12, 2735–2771, https://doi.org/10.5194/se-12-2735-2021, https://doi.org/10.5194/se-12-2735-2021, 2021
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Molasse deposits, deposited and deformed at the western Alpine front during the Miocene (23 to 5.6 Ma), record the chronology of that deformation. We combine the first precise chronostratigraphy (precision of ∼0.5 Ma) of the Miocene molasse, the reappraisal of the regional structure, and the analysis of growth deformation structures in order to document three tectonic phases and the precise chronology of thrust westward propagation during the second one involving the Belledonne basal thrust.
Mark R. Handy, Stefan M. Schmid, Marcel Paffrath, Wolfgang Friederich, and the AlpArray Working Group
Solid Earth, 12, 2633–2669, https://doi.org/10.5194/se-12-2633-2021, https://doi.org/10.5194/se-12-2633-2021, 2021
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New images from the multi-national AlpArray experiment illuminate the Alps from below. They indicate thick European mantle descending beneath the Alps and forming blobs that are mostly detached from the Alps above. In contrast, the Adriatic mantle in the Alps is much thinner. This difference helps explain the rugged mountains and the abundance of subducted and exhumed units at the core of the Alps. The blobs are stretched remnants of old ocean and its margins that reach down to at least 410 km.
Maurizio Ercoli, Daniele Cirillo, Cristina Pauselli, Harry M. Jol, and Francesco Brozzetti
Solid Earth, 12, 2573–2596, https://doi.org/10.5194/se-12-2573-2021, https://doi.org/10.5194/se-12-2573-2021, 2021
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Past strong earthquakes can produce topographic deformations, often
memorizedin Quaternary sediments, which are typically studied by paleoseismologists through trenching. Using a ground-penetrating radar (GPR), we unveiled possible buried Quaternary faulting in the Mt. Pollino seismic gap region (southern Italy). We aim to contribute to seismic hazard assessment of an area potentially prone to destructive events as well as promote our workflow in similar contexts around the world.
Luca Smeraglia, Nathan Looser, Olivier Fabbri, Flavien Choulet, Marcel Guillong, and Stefano M. Bernasconi
Solid Earth, 12, 2539–2551, https://doi.org/10.5194/se-12-2539-2021, https://doi.org/10.5194/se-12-2539-2021, 2021
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In this paper, we dated fault movements at geological timescales which uplifted the sedimentary successions of the Jura Mountains from below the sea level up to Earth's surface. To do so, we applied the novel technique of U–Pb geochronology on calcite mineralizations that precipitated on fault surfaces during times of tectonic activity. Our results document a time frame of the tectonic evolution of the Jura Mountains and provide new insight into the broad geological history of the Western Alps.
Renas I. Koshnaw, Fritz Schlunegger, and Daniel F. Stockli
Solid Earth, 12, 2479–2501, https://doi.org/10.5194/se-12-2479-2021, https://doi.org/10.5194/se-12-2479-2021, 2021
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As continental plates collide, mountain belts grow. This study investigated the provenance of rocks from the northwestern segment of the Zagros mountain belt to unravel the convergence history of the Arabian and Eurasian plates. Provenance data synthesis and field relationships suggest that the Zagros Mountains developed as a result of the oceanic crust emplacement on the Arabian continental plate, followed by the Arabia–Eurasia collision and later uplift of the broader region.
David Hindle and Jonas Kley
Solid Earth, 12, 2425–2438, https://doi.org/10.5194/se-12-2425-2021, https://doi.org/10.5194/se-12-2425-2021, 2021
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Central western Europe underwent a strange episode of lithospheric deformation, resulting in a chain of small mountains that run almost west–east across the continent and that formed in the middle of a tectonic plate, not at its edges as is usually expected. Associated with these mountains, in particular the Harz in central Germany, are marine basins contemporaneous with the mountain growth. We explain how those basins came to be as a result of the mountains bending the adjacent plate.
Andreas Eberts, Hamed Fazlikhani, Wolfgang Bauer, Harald Stollhofen, Helga de Wall, and Gerald Gabriel
Solid Earth, 12, 2277–2301, https://doi.org/10.5194/se-12-2277-2021, https://doi.org/10.5194/se-12-2277-2021, 2021
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We combine gravity anomaly and topographic data with observations from thermochronology, metamorphic grades, and the granite inventory to detect patterns of basement block segmentation and differential exhumation along the southwestern Bohemian Massif. Based on our analyses, we introduce a previously unknown tectonic structure termed Cham Fault, which, together with the Pfahl and Danube shear zones, is responsible for the exposure of different crustal levels during late to post-Variscan times.
Christoph Grützner, Simone Aschenbrenner, Petra Jamšek
Rupnik, Klaus Reicherter, Nour Saifelislam, Blaž Vičič, Marko Vrabec, Julian Welte, and Kamil Ustaszewski
Solid Earth, 12, 2211–2234, https://doi.org/10.5194/se-12-2211-2021, https://doi.org/10.5194/se-12-2211-2021, 2021
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Several large strike-slip faults in western Slovenia are known to be active, but most of them have not produced strong earthquakes in historical times. In this study we use geomorphology, near-surface geophysics, and fault excavations to show that two of these faults had surface-rupturing earthquakes during the Holocene. Instrumental and historical seismicity data do not capture the strongest events in this area.
Michael Warsitzka, Prokop Závada, Fabian Jähne-Klingberg, and Piotr Krzywiec
Solid Earth, 12, 1987–2020, https://doi.org/10.5194/se-12-1987-2021, https://doi.org/10.5194/se-12-1987-2021, 2021
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A new analogue modelling approach was used to simulate the influence of tectonic extension and tilting of the basin floor on salt tectonics in rift basins. Our results show that downward salt flow and gravity gliding takes place if the flanks of the rift basin are tilted. Thus, extension occurs at the basin margins, which is compensated for by reduced extension and later by shortening in the graben centre. These outcomes improve the reconstruction of salt-related structures in rift basins.
Steffen Ahlers, Andreas Henk, Tobias Hergert, Karsten Reiter, Birgit Müller, Luisa Röckel, Oliver Heidbach, Sophia Morawietz, Magdalena Scheck-Wenderoth, and Denis Anikiev
Solid Earth, 12, 1777–1799, https://doi.org/10.5194/se-12-1777-2021, https://doi.org/10.5194/se-12-1777-2021, 2021
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Knowledge about the stress state in the upper crust is of great importance for many economic and scientific questions. However, our knowledge in Germany is limited since available datasets only provide pointwise, incomplete and heterogeneous information. We present the first 3D geomechanical model that provides a continuous description of the contemporary crustal stress state for Germany. The model is calibrated by the orientation of the maximum horizontal stress and stress magnitudes.
Torsten Hundebøl Hansen, Ole Rønø Clausen, and Katrine Juul Andresen
Solid Earth, 12, 1719–1747, https://doi.org/10.5194/se-12-1719-2021, https://doi.org/10.5194/se-12-1719-2021, 2021
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We have analysed the role of deep salt layers during tectonic shortening of a group of sedimentary basins buried below the North Sea. Due to the ability of salt to flow over geological timescales, the salt layers are much weaker than the surrounding rocks during tectonic deformation. Therefore, complex structures formed mainly where salt was present in our study area. Our results align with findings from other basins and experiments, underlining the importance of salt tectonics.
Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs
Solid Earth, 12, 1473–1495, https://doi.org/10.5194/se-12-1473-2021, https://doi.org/10.5194/se-12-1473-2021, 2021
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We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.
Laurent Jolivet, Laurent Arbaret, Laetitia Le Pourhiet, Florent Cheval-Garabédian, Vincent Roche, Aurélien Rabillard, and Loïc Labrousse
Solid Earth, 12, 1357–1388, https://doi.org/10.5194/se-12-1357-2021, https://doi.org/10.5194/se-12-1357-2021, 2021
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Although viscosity of the crust largely exceeds that of magmas, we show, based on the Aegean and Tyrrhenian Miocene syn-kinematic plutons, how the intrusion of granites in extensional contexts is controlled by crustal deformation, from magmatic stage to cold mylonites. We show that a simple numerical setup with partial melting in the lower crust in an extensional context leads to the formation of metamorphic core complexes and low-angle detachments reproducing the observed evolution of plutons.
Miguel Cisneros, Jaime D. Barnes, Whitney M. Behr, Alissa J. Kotowski, Daniel F. Stockli, and Konstantinos Soukis
Solid Earth, 12, 1335–1355, https://doi.org/10.5194/se-12-1335-2021, https://doi.org/10.5194/se-12-1335-2021, 2021
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Constraining the conditions at which rocks form is crucial for understanding geologic processes. For years, the conditions under which rocks from Syros, Greece, formed have remained enigmatic; yet these rocks are fundamental for understanding processes occurring at the interface between colliding tectonic plates (subduction zones). Here, we constrain conditions under which these rocks formed and show they were transported to the surface adjacent to the down-going (subducting) tectonic plate.
Karsten Reiter
Solid Earth, 12, 1287–1307, https://doi.org/10.5194/se-12-1287-2021, https://doi.org/10.5194/se-12-1287-2021, 2021
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The influence and interaction of elastic material properties (Young's modulus, Poisson's ratio), density and low-friction faults on the resulting far-field stress pattern in the Earth's crust is tested with generic models. A Young's modulus contrast can lead to a significant stress rotation. Discontinuities with low friction in homogeneous models change the stress pattern only slightly, away from the fault. In addition, active discontinuities are able to compensate stress rotation.
Anthony Jourdon, Charlie Kergaravat, Guillaume Duclaux, and Caroline Huguen
Solid Earth, 12, 1211–1232, https://doi.org/10.5194/se-12-1211-2021, https://doi.org/10.5194/se-12-1211-2021, 2021
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The borders between oceans and continents, called margins, can be convergent, divergent, or horizontally sliding. The formation of oceans occurs in a divergent context. However, some divergent margin structures display an accommodation of horizontal sliding during the opening of oceans. To study and understand how the horizontal sliding part occurring during divergence influences the margin structure, we performed 3D high-resolution numerical models evolving during tens of millions of years.
Maria Francesca Ferrario and Franz Livio
Solid Earth, 12, 1197–1209, https://doi.org/10.5194/se-12-1197-2021, https://doi.org/10.5194/se-12-1197-2021, 2021
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Moderate to strong earthquakes commonly produce surface faulting, either along the primary fault or as distributed rupture on nearby faults. Hazard assessment for distributed normal faulting is based on empirical relations derived almost 15 years ago. In this study, we derive updated empirical regressions of the probability of distributed faulting as a function of distance from the primary fault, and we propose a conservative scenario to consider the full spectrum of potential rupture.
Hilmar von Eynatten, Jonas Kley, István Dunkl, Veit-Enno Hoffmann, and Annemarie Simon
Solid Earth, 12, 935–958, https://doi.org/10.5194/se-12-935-2021, https://doi.org/10.5194/se-12-935-2021, 2021
Eline Le Breton, Sascha Brune, Kamil Ustaszewski, Sabin Zahirovic, Maria Seton, and R. Dietmar Müller
Solid Earth, 12, 885–913, https://doi.org/10.5194/se-12-885-2021, https://doi.org/10.5194/se-12-885-2021, 2021
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The former Piemont–Liguria Ocean, which separated Europe from Africa–Adria in the Jurassic, opened as an arm of the central Atlantic. Using plate reconstructions and geodynamic modeling, we show that the ocean reached only 250 km width between Europe and Adria. Moreover, at least 65 % of the lithosphere subducted into the mantle and/or incorporated into the Alps during convergence in Cretaceous and Cenozoic times comprised highly thinned continental crust, while only 35 % was truly oceanic.
Xiong Ou, Anne Replumaz, and Peter van der Beek
Solid Earth, 12, 563–580, https://doi.org/10.5194/se-12-563-2021, https://doi.org/10.5194/se-12-563-2021, 2021
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The low-relief, mean-elevation Baima Xueshan massif experienced slow exhumation at a rate of 0.01 km/Myr since at least 22 Ma and then regional rock uplift at 0.25 km/Myr since ~10 Ma. The high-relief, high-elevation Kawagebo massif shows much stronger local rock uplift related to the motion along a west-dipping thrust fault, at a rate of 0.45 km/Myr since at least 10 Ma, accelerating to 1.86 km/Myr since 1.6 Ma. Mekong River incision plays a minor role in total exhumation in both massifs.
Jack N. Williams, Hassan Mdala, Åke Fagereng, Luke N. J. Wedmore, Juliet Biggs, Zuze Dulanya, Patrick Chindandali, and Felix Mphepo
Solid Earth, 12, 187–217, https://doi.org/10.5194/se-12-187-2021, https://doi.org/10.5194/se-12-187-2021, 2021
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Earthquake hazard is often specified using instrumental records. However, this record may not accurately forecast the location and magnitude of future earthquakes as it is short (100s of years) relative to their frequency along geologic faults (1000s of years). Here, we describe an approach to assess this hazard using fault maps and GPS data. By applying this to southern Malawi, we find that its faults may host rare (1 in 10 000 years) M 7 earthquakes that pose a risk to its growing population.
Lior Suchoy, Saskia Goes, Benjamin Maunder, Fanny Garel, and Rhodri Davies
Solid Earth, 12, 79–93, https://doi.org/10.5194/se-12-79-2021, https://doi.org/10.5194/se-12-79-2021, 2021
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We use 2D numerical models to highlight the role of basal drag in subduction force balance. We show that basal drag can significantly affect velocities and evolution in our simulations and suggest an explanation as to why there are no trends in plate velocities with age in the Cenozoic subduction record (which we extracted from recent reconstruction using GPlates). The insights into the role of basal drag will help set up global models of plate dynamics or specific regional subduction models.
William Bosworth and Gábor Tari
Solid Earth, 12, 59–77, https://doi.org/10.5194/se-12-59-2021, https://doi.org/10.5194/se-12-59-2021, 2021
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Many of the world's hydrocarbon resources are found in rifted sedimentary basins. Some rifts experience multiple phases of extension and inversion. This results in complicated oil and gas generation, migration, and entrapment histories. We present examples of basins in the Western Desert of Egypt and the western Black Sea that were inverted multiple times, sometimes separated by additional phases of extension. We then discuss how these complex deformation histories impact exploration campaigns.
Samuel Mock, Christoph von Hagke, Fritz Schlunegger, István Dunkl, and Marco Herwegh
Solid Earth, 11, 1823–1847, https://doi.org/10.5194/se-11-1823-2020, https://doi.org/10.5194/se-11-1823-2020, 2020
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Based on thermochronological data, we infer thrusting along-strike the northern rim of the Central Alps between 12–4 Ma. While the lithology influences the pattern of thrusting at the local scale, we observe that thrusting in the foreland is a long-wavelength feature occurring between Lake Geneva and Salzburg. This coincides with the geometry and dynamics of the attached lithospheric slab at depth. Thus, thrusting in the foreland is at least partly linked to changes in slab dynamics.
Simon Preuss, Jean Paul Ampuero, Taras Gerya, and Ylona van Dinther
Solid Earth, 11, 1333–1360, https://doi.org/10.5194/se-11-1333-2020, https://doi.org/10.5194/se-11-1333-2020, 2020
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In this paper, we present newly developed numerical models to simulate episodic growth of geological faults.
This growth of faults occurs during the seismic cycle, with spontaneously generated primary and secondary fault structures. With these models we are able to show the evolution of complex fault geometries. Additionally, we can quantify the impact of earthquakes on fault growth.
Paul Angrand, Frédéric Mouthereau, Emmanuel Masini, and Riccardo Asti
Solid Earth, 11, 1313–1332, https://doi.org/10.5194/se-11-1313-2020, https://doi.org/10.5194/se-11-1313-2020, 2020
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We study the Iberian plate motion, from the late Permian to middle Cretaceous. During this time interval, two oceanic systems opened. Geological evidence shows that the Iberian domain preserved the propagation of these two rift systems well. We use geological evidence and pre-existing kinematic models to propose a coherent kinematic model of Iberia that considers both the Neotethyan and Atlantic evolutions. Our model shows that the Europe–Iberia plate boundary was made of two rift systems.
Daniel Pastor-Galán, Gabriel Gutiérrez-Alonso, and Arlo B. Weil
Solid Earth, 11, 1247–1273, https://doi.org/10.5194/se-11-1247-2020, https://doi.org/10.5194/se-11-1247-2020, 2020
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Pangea was assembled during Devonian to early Permian times and resulted in a large-scale and winding orogeny that today transects Europe, northwestern Africa, and eastern North America. This orogen is characterized by an
Sshape corrugated geometry in Iberia. This paper presents the advances and milestones in our understanding of the geometry and kinematics of the Central Iberian curve from the last decade with particular attention paid to structural and paleomagnetic studies.
Richard Spitz, Arthur Bauville, Jean-Luc Epard, Boris J. P. Kaus, Anton A. Popov, and Stefan M. Schmalholz
Solid Earth, 11, 999–1026, https://doi.org/10.5194/se-11-999-2020, https://doi.org/10.5194/se-11-999-2020, 2020
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We apply three-dimensional (3D) thermo-mechanical numerical simulations of the shortening of the upper crustal region of a passive margin in order to investigate the control of 3D laterally variable inherited structures on fold-and-thrust belt evolution and associated nappe formation. The model is applied to the Helvetic nappe system of the Swiss Alps. Our results show a 3D reconstruction of the first-order tectonic evolution showing the fundamental importance of inherited geological structures.
Manfred Lafosse, Elia d'Acremont, Alain Rabaute, Ferran Estrada, Martin Jollivet-Castelot, Juan Tomas Vazquez, Jesus Galindo-Zaldivar, Gemma Ercilla, Belen Alonso, Jeroen Smit, Abdellah Ammar, and Christian Gorini
Solid Earth, 11, 741–765, https://doi.org/10.5194/se-11-741-2020, https://doi.org/10.5194/se-11-741-2020, 2020
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The Alboran Sea is one of the most active region of the Mediterranean Sea. There, the basin architecture records the effect of the Africa–Eurasia plates convergence. We evidence a Pliocene transpression and a more recent Pleistocene tectonic reorganization. We propose that main driving force of the deformation is the Africa–Eurasia convergence, rather than other geodynamical processes. It highlights the evolution and the geometry of the present-day Africa–Eurasia plate boundary.
Dan J. Clark, Sarah Brennand, Gregory Brenn, Matthew C. Garthwaite, Jesse Dimech, Trevor I. Allen, and Sean Standen
Solid Earth, 11, 691–717, https://doi.org/10.5194/se-11-691-2020, https://doi.org/10.5194/se-11-691-2020, 2020
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A magnitude 5.3 reverse-faulting earthquake in September 2018 near Lake Muir in southwest Western Australia was followed after 2 months by a collocated magnitude 5.2 strike-slip event. The first event produced a ~ 5 km long and up to 0.5 m high west-facing surface rupture, and the second triggered event deformed but did not rupture the surface. The earthquake sequence was the ninth to have produced surface rupture in Australia. None of these show evidence for prior Quaternary surface rupture.
Craig Magee and Christopher Aiden-Lee Jackson
Solid Earth, 11, 579–606, https://doi.org/10.5194/se-11-579-2020, https://doi.org/10.5194/se-11-579-2020, 2020
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Injection of vertical sheets of magma (dyke swarms) controls tectonic and volcanic processes on Earth and other planets. Yet we know little of the 3D structure of dyke swarms. We use seismic reflection data, which provides ultrasound-like images of Earth's subsurface, to study a dyke swarm in 3D for the first time. We show that (1) dyke injection occurred in the Late Jurassic, (2) our data support previous models of dyke shape, and (3) seismic data provides a new way to view and study dykes.
Cited articles
Abbott, M. J. and Chamalaun, F. H.: Geochronology of some Banda Arc Volcanics, in: The Geology and Tectonics of Eastern Indonesia, edited by: Barber, A. J. and Wiryusujono, S., Geological Research and Development Centre, Special Publication, 2, 253–268, Bandung, 1981.
Acosta-Vigil, A., Buick, I., Hermann, J., Cesare, B., Rubatto, D., London, D., and Morgan, G. B.: Mechanisms of crustal anatexis: a geochemical study of partially melted metapelitic enclaves and host dacite, SE Spain, J. Petrol., 51, 785–821, https://doi.org/10.1093/petrology/egp095, 2010.
Afiri, A., Gueydan, F., Pitra, P., Essaifi, A., and Précigout, J.: Oligo-Miocene exhumation of the Beni-Bousera peridotite through a lithosphere-scale extensional shear zone, Geodin. Acta, 24, 49–60, https://doi.org/10.3166/ga.24.49-60, 2011.
Álvarez-Valero, A. M. and Waters, D. J.: Partially melted crustal xenoliths as a window into sub-volcanic processes: Evidence from the Neogene Magmatic Province of the Betic Cordillera, SE Spain, J. Petrol., 51, 973–991, https://doi.org/10.1093/petrology/egq007, 2010.
Audley-Charles, M. G.: Tectonic post-collision processes in Timor, in: The SE Asian Gateway: History and Tectonics of the Australia-Asia Collision, edited by: Hall, R., Cottam, M. A., and Wilson, M. E. J., Geol. Soc., London, Spec. Pub., 355, 241–266, https://doi.org/10.1144/SP355.12, 2011.
Audley-Charles, M. G., Carter, D. J., and Milsom, J. S.: Tectonic development of Eastern Indonesia in relation to Gondwanaland dispersal, Nature, 239, 35–39, https://doi.org/10.1038/physci239035a0, 1972.
Audley-Charles, M. G., Carter, D. J., Barber, A. J., Norvick, M. S., and Tjokrosapoetro, S.: Reinterpretation of the geology of Seram: implications for the Banda Arcs and northern Australia, J. Geol. Soc. London, 136, 547–566, https://doi.org/10.1144/gsjgs.136.5.0547, 1979.
Bachri, S.: Tectonostratigraphy and structures of eastern Seram, J. Geol. Indonesia, 6, 85–93, 2011.
Barber, A. J., Tjokrosapoetro, S., and Charlton, T. R.: Mud volcanoes, shale diapirs, wrench faults and melanges in accretionary complexes, Eastern Indonesia, AAPG Bull., 70, 1729–1741, 1986.
Beckinsale, R. and Nakapadungrat, S.: A late Miocene K-Ar age for the lavas of Pulau Kelang, Seram, Indonesia, J. Phys. Earth, 26, 199–201, 1978.
Bock, Y., Prawirodirdjo, L., Genrich J. F., Stevens, C. W., McCaffrey R., Subarya C., Puntodewo S. S. O., and Calais W.: Crustal motion in Indonesia from Global Positioning System measurements, J. Geophys. Res., 108, 2367, https://doi.org/10.1029/2001JB000324, 2003.
Boudier, F. and Nicolas, A.: Harzburgite and lherzolite subtypes in ophiolitic and oceanic environments, Earth Planet Sc. Lett., 76, 84–92, 1985.
Bowin, C., Purdy, G. M., Johnston, C., Shor, G., Lawver, L., Hartono, H. M. S., and Jezek, P.: Arc-Continent collision in Banda Sea region, AAPG Bull., 64, 868–915, 1980.
Brouwer, H. A.: Geologische onderzoekingen in Oost-Ceram, Tijd. K. Ned. Aardr. Gen., 36, 715–751, 1919.
Brouwer, H. A.: Over insluitsels en cordierietgehalte van bronziet-dacieten van het eiland Ambon, Verhand. Geol. Mijnb. Gen. Nederland. Kol., Geol. Ser. VIII, 73–80, 1925.
Cardwell, R. K. and Isacks, B. L.: Geometry of the subducted lithosphere beneath the Banda Sea in eastern Indonesia from seismicity and fault plane solutions, J. Geophys. Res., 83, 2825–2838, https://doi.org/10.1029/JB083iB06p02825, 1978.
Charlton, T. R.: Correlation of the Salawati and Tomori Basins, eastern Indonesia: a constraint on left-lateral displacements of the Sorong fault zone, in: Tectonic Evolution of Southeast Asia, edited by: Hall, R. and Blundell, D., Geol. Soc. London Spec. Pub., 106, 465–481, https://doi.org/10.1144/GSL.SP.1996.106.01.29, 1996.
Charlton, T. R.: The petroleum potential of inversion anticlines in the Banda Arc, AAPG Bull., 88, 565–585, https://doi.org/10.1306/12290303055, 2004.
Darman, H. and Reemst, P.: Seismic expression of geological features in Seram Sea: Seram Trough , Misool-Onin Ridge and Sedimentary Basin, Berita Sedimentol., 23, 28–34, 2012.
Das, S.: Seismicity gaps and the shape of the seismic zone in the Banda Sea region from relocated hypocenters, J. Geophys. Res., 109, B12303, https://doi.org/10.1029/2004JB003192, 2004.
Dasgupta, S., Sengupta, P., Ehl, J., Raith, M., and Bardhan, S.: Reaction textures in a suite of spinel granulites from the Eastern Ghats Belt, India: Evidence for polymetamorphism, a partial petrogenetic Grid in the system KFMASH and the roles of ZnO and Fe2O3, J. Petrol., 36, 435–461, 1995.
de Jong, H.: Studien uber Eruptiv- und Mischgesteine des Kaibobogebietes, Geol. Petrogr. and Pal. Results of Explorations in the Isle of Ceram, 1, 1923.
de Smet, M. E. M.: A geometrically consistent plate-tectonic model for eastern Indonesia, Neth. J. Sea Res., 24, 173–183, https://doi.org/10.1016/0077-7579(89)90148-8, 1989.
de Smet, M. E. M. and Barber, A. J.: Report on the Geology of Seram (Unpublished Report), Geological Research in Southeast Asia, University of London, UK, 1992.
de Smet, M. E. M., Fortuin, A., Tjokrosapoetro, S., and van Hinte, J.: Late Cenozoic vertical movements of non-volcanic islands in the Banda Arc area, Neth. J. Sea Res., 24, 263–275, https://doi.org/10.1016/0077-7579(89)90153-1, 1989a.
de Smet, M. E. M., Sumosusastro, P. A., Siregar, I., Van Marle, L. J., Troelstra, S. R., and Fortuin, A. R.: Late Cenozoic stratigraphy and tectonics of Seram, Indonesia, Geol. Mijnbouw, 68, 221–235, 1989b.
Deninger, K.: Geographische Ubersicht vom West-Seran, Petermann Geogr. Mitt, 385–388, 1915.
Deninger, K.: Zur Geologie von Mittel-Seran (Ceram), Palaeontographica, Suppl. IV, Beitr. Geologie Niederlandisch-Inden III, 2, 25–58, 1918.
Doblas, M. and Oyarzun, R.: "Mantle core complexes" and Neogene extensional detachment tectonics in the western Betic Cordilleras, Spain: an alternative model for the emplacement of the Ronda peridotite, Earth Planet. Sc. Lett., 93, 76–84, https://doi.org/10.1016/0012-821X(89)90185-4, 1989.
Fichtner, A., Kennett, B. L., Igel, H., and Bunge, H.-P.: Full waveform tomography for radially anisotropic structure: New insights into present and past states of the Australasian upper mantle, Earth Planet. Sc. Lett., 290, 270–280, https://doi.org/10.1016/j.epsl.2009.12.003, 2010.
Gafoer, S., Suwitodirdjo, K., and Suharsono: Geological map of the Bula and Watubela sheet, Maluku, 1:250000, Geological Research and Development Centre, Bandung, Indonesia, 1993.
Germeraad, J. H.: Geology of central Seran, in: Geological, petrographical, and palaeontological results of explorations, carried out from September 1917 till June 1919 in the island of Ceram, edited by: Rutten, L. and Hotz, W., 2, 135 pp., De Bussy, Amsterdam, 1946.
Haile, N. S.: Paleomagnetic evidence for the rotation of Seram, Indonesia, J. Phys. Earth, 26, 191–198, 1978.
Hall, R.: Reconstructing Cenozoic SE Asia, in: Tectonic Evolution of Southeast Asia, edited by: Hall, R. and Blundell, D., Geol. Soc. London Spec. Pub., 106, 153–184, https://doi.org/10.1144/GSL.SP.1996.106.01.11, 1996.
Hall, R.: Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations, J. Asian Earth Sci., 20, 353–431, https://doi.org/10.1016/S1367-9120(01)00069-4, 2002.
Hall, R.: Australia-SE Asia collision: plate tectonics and crustal flow, in: The SE Asian Gateway: History and Tectonics of the Australia-Asia Collision, edited by: Hall, R., Cottam, M. A., and Wilson, M. E. J., Geol. Soc. London Spec. Pub., 355, 75–109, https://doi.org/10.1144/SP355.5, 2011.
Hall, R.: Late Jurassic-Cenozoic reconstructions of the Indonesian region and the Indian Ocean, Tectonophysics, 570–571, 1–41, https://doi.org/10.1016/j.tecto.2012.04.021, 2012.
Hall, R. and Sevastjanova, I.: Australian crust in Indonesia, Aust. J. Earth Sci., 59, 827–844, https://doi.org/10.1080/08120099.2012.692335, 2012.
Hall, R. and Wilson, M. E. J.: Neogene sutures in eastern Indonesia, J. Asian Earth Sci., 18, 781–808, 2000.
Hamilton, W.: Tectonics of the Indonesian Region, USGS Professional Paper, 1078, 345, 1979.
Harley, S. L.: Refining the P-T records of UHT crustal metamorphism, J. Metamorph. Geol., 26, 125–154, https://doi.org/10.1111/j.1525-1314.2008.00765.x, 2008.
Harris, R.: Rise and fall of the Eastern Great Indonesian arc recorded by the assembly, dispersion and accretion of the Banda Terrane, Timor, Gondwana Res., 10, 207–231, https://doi.org/10.1016/j.gr.2006.05.010, 2006.
Helmers, H., Sopaheluwakan, J., Tjokrosapoetro, S., and Nila, E.: High-grade metamorphism related to peridotite emplacement near Atapupu, Timor with reference to the Kaibobo peridotite on Seram, Indonesia, Neth. J. Sea Res., 24, 357–371, https://doi.org/10.1016/0077-7579(89)90161-0, 1989.
Hill, K. C.: Tectonics and regional structure of Seram and the Banda Arc, Proceedings, Indonesian Petroleum Association, 30, 559–578, 2005.
Hinschberger, F., Malod, J., Rehault, J., Villeneuve, M., Royer, J., and Burhanuddin, S.: Late Cenozoic geodynamic evolution of eastern Indonesia, Tectonophysics, 404, 91–118, https://doi.org/10.1016/j.tecto.2005.05.005, 2005.
Honthaas, C., Maury, R., Priadi, B., Bellon, H., and Cotten, J.: The Plio–Quaternary Ambon arc, Eastern Indonesia, Tectonophysics, 301, 261–281, https://doi.org/10.1016/S0040-1951(98)00227-3, 1999.
Hutchison, C. S.: Discussion of Carter, D. J. et al., 1976, in: Proceedings: Society Meetings September–December 1975, J. Geol. Soc. London, 358–61, 1976.
John, R. and Barber, A. J.: Structure and stratigraphy of the Bula area, Seram. Report of fieldwork programme, October–November 1989 (Unpublished Report), Geological Research in Southeast Asia, University of London, 1990.
Katili, J. A.: Volcanism and plate tectonics in the Indonesian island arcs, Tectonophysics, 26, 165–188, 1975.
Katili, J. A.: Review of past and present geotectonic concepts of Eastern Indonesia, Neth. J. Sea Res., 24, 103–129, 1989.
Kelsey, D. E.: On ultrahigh-temperature crustal metamorphism, Gondwana Res., 13, 1–29, https://doi.org/10.1016/j.gr.2007.06.001, 2008.
Kemp, G. and Mogg, W.: A reappraisal of the geology, tectonics and prospectivity of Seram Island, Eastern Indonesia, Proc. Indonesian Petr. Assoc., 21, 521–552, 1992.
Krumbeck, L.: Geologische Ergebnisse der Reisen K. Deninger's in den Molukken. III. Brachiopoden, Lamellibranchiaten und Gastropoden aus der oberen Trias der Insel Seram (Mittel-Seram), Palaeontographica, Suppl. IV, Beitr. Geologie Niederlandisch-Inden III, 5, 185–246, 1922.
Lal, R. K., Ackermand, D., and Upadhyay, H.: P-T-X relationships deduced from corona textures in sapphirine-spinel-quartz assemblages from Paderu, Southern India, J. Petrol., 28, 1139–1168, 1987.
Linthout, K. and Helmers, H.: Pliocene obducted, rotated and migrated ultramafic rocks and obduction-induced anatectic granite, SW Seram and Ambon, Eastern Indonesia, J. SE Asian Earth Sci., 9, 95–109, https://doi.org/10.1016/0743-9547(94)90068-X, 1994.
Linthout, K., Helmers, H., Sopaheluwakan, J., and Nila, E. S.: Metamorphic complexes in Buru and Seram, northern Banda Arc, Neth. J. Sea Res., 24, 345–356, 1989.
Linthout, K., Helmers, H., and Andriessen, P.: Dextral strike-slip in Central Seram and 3–4.5 Ma Rb/Sr ages in pre-Triassic metamorphics related to Early Pliocene counterclockwise rotation of the Buru-Seram microplate (E. Indonesia), J. SE Asian Earth Sci., 6, 335–342, https://doi.org/10.1016/0743-9547(91)90079-D, 1991.
Linthout, K., Helmers, H., Wijbrans, J. R., and Van Wees, J. D. A. M.: 40Ar/39Ar constraints on obduction of the Seram ultramafic complex: consequences for the evolution of the southern Banda Sea, in: Tectonic Evolution of Southeast Asia, edited by: Hall, R. and Blundell, D., Geol. Soc. London Spec. Pub., 106, 455–464, https://doi.org/10.1144/GSL.SP.1996.106.01.28, 1996.
Linthout, K., Helmers, H., and Sopaheluwakan, J.: Late Miocene obduction and microplate migration around the southern Banda Sea and the closure of the Indonesian Seaway, Tectonophysics, 281, 17–30, https://doi.org/10.1016/S0040-1951(97)00156-X, 1997.
Long, K. L.: Preliminary descriptive deposit model for detachment-fault-related mineralization, US Geol. Surv. Bull., 2004, 52–62, 1992.
Martin, K.: Over de geologie van West-Seran (Ceram), Handeling 8e Nederl. Natuur Geneesk. Congres., Rotterdam, 301–303, 1901.
Martini, R., Zaninetti, L., Lathuillière, B., Cirilli, S., Cornée, J. J., and Villeneuve, M.: Upper Triassic carbonate deposits of Seram (Indonesia): palaeogeographic and geodynamic implications, Palaeogeogr. Palaeocl., 206, 75–102, https://doi.org/10.1016/j.palaeo.2003.12.020, 2004.
McCaffrey, R.: Active tectonics of the eastern Sunda and Banda arcs, J. Geophys. Res., 93, 163–182, 1988.
McCaffrey, R.: Seismological contraints and speculations on Banda Arc tectonics, Neth. J. Sea Res., 24, 141–152, 1989.
McCaffrey, R., Silver, E. A., and Rait, R. W.: Crustal structure of the Molucca Sea collision zone, Indonesia, in: The tectonic and geologic evolution of south-east Asian seas and islands, edited by: Hayes, D. E., American Geophysical Union, 23, 161–177, 1980.
Milsom, J.: Preliminary gravity map of Seram, eastern Indonesia, Geology, 5, 641–643, 1977.
Milsom, J.: Subduction in eastern Indonesia: how many slabs?, Tectonophysics, 338, 167–178, https://doi.org/10.1016/S0040-1951(01)00137-8, 2001.
Milsom, J., Sardjono, and Susilo, A.: Short-wavelength, high-amplitude gravity anomalies around the Banda Sea, and the collapse of the Sulawesi orogen, Tectonophysics, 333, 61–74, https://doi.org/10.1016/S0040-1951(00)00267-5, 2001.
Milsom, J. S.: Origin of the Uliasser Islands, eastern Indonesia, J. Geol. Soc. London, 136, 581–582, https://doi.org/10.1144/gsjgs.136.5.0581, 1979.
Monnier, C., Girardeau, J., Permana, H., Rehault, J.-P., Bellon, H., and Cotten, J.: Dynamics and age of formation of the Seram-Ambon ophiolites (Central Indonesia), B. Soc. Geol. Fr., 174, 529–543, https://doi.org/10.2113/174.6.529, 2003.
Morales, J., Serrano, I., Jabaloy, A., Galindo-Zaldívar, J., Zhao, D., Torcal, F., Vidal, F., and González-Lodeiro, F.: Active continental subduction beneath the Betic Cordillera and the Alborán Sea, Geology, 27, 735, https://doi.org/10.1130/0091-7613(1999)027<0735:ACSBTB>2.3.CO;2, 1999.
Morimoto, T., Santosh, M., Tsunogae, T., and Yoshimura, Y.: Spinel + Quartz association from the Kerala khondalites, southern India: evidence for ultrahigh temperature metamorphism, J. Miner. Petrol. Sci., 99, 257–278, 2004.
Nebel, O., Vroon, P., van Westrenen, W., Iizuka, T., and Davies, G.: The effect of sediment recycling in subduction zones on the Hf isotope character of new arc crust, Banda arc, Indonesia, Earth Planet. Sc. Lett., 303, 240–250, https://doi.org/10.1016/j.epsl.2010.12.053, 2011.
Nugroho, H., Harris, R., Lestariya, A. W., and Maruf, B.: Plate boundary reorganization in the active Banda Arc-continent collision: Insights from new GPS measurements, Tectonophysics, 479, 52–65, https://doi.org/10.1016/j.tecto.2009.01.026, 2009.
O'Sullivan, T., Pegum, D., and Tarigan, J.: Seram oil search, Past discoveries and future oil potential, Proc. Indones. Petrol. Assoc., 14, 3–20, 1985.
Ouzegane, K. and Boumaza, S.: An example of ultrahigh-temperature metamorphism: orthopyroxene-sillimanite-garnet, sapphirine-quartz and spinel-quartz parageneses in Al-Mg granulites from In Hihaou, In Ouzzal, Hoggar, J. Metamorph. Geol., 14, 693–708, 1996.
Pairault, A. A., Hall, R., and Elders, C. F.: Structural styles and tectonic evolution of the Seram Trough, Indonesia, Mar. Petrol. Geol., 20, 1141–1160, https://doi.org/10.1016/j.marpetgeo.2003.10.001, 2003a.
Pairault, A. A., Hall, R., and Elders, C. F.: Tectonic evolution of the Seram Trough, Indonesia, Proc. Indones. Petrol. Assoc., 29, 355–370, 2003b.
Papaioannou, A.: Structure and stratigraphy of central and eastern Seram: Fieldwork Report (Unpublished Report), Geological Research in Southeast Asia, University of London, 1991.
Pieters, P. E., Pigram, C. J., Trail, D. S., Dow, D. B., Ratman, N., Sukamto, R.: The stratigraphy of western Irian Jaya, B. Indones. Geol. Res. Dev. Cent., 8, 14–48, 1983.
Pownall, J. M., Hall, R., and Watkinson, I. M.: Intrusive peridotites and granites exhumed on Seram and Ambon, eastern Indonesia, during Banda Arc subduction rollback, Tectonic Studies Group AGM 2012, Edinburgh, UK, 4–6 January 2012, 2012a.
Pownall, J. M., Hall, R., and Watkinson, I. M.: Ultra-high temperature metamorphism and anatexis linked to mantle exhumation on Seram, eastern Indonesia, Metamorphic Studies Group Research-in-Progress Meeting 2012, Cambridge, UK, 21 March 2012, 2012b.
Pownall, J. M., Hall, R., Watkinson, I. M., and Forster, M.: Pliocene Mantle Exhumation, granulite facies Metamorphism, and Anatexis driven by Banda Arc Slab Rollback beneath Seram, Eastern Indonesia, 2012 Fall Meeting, AGU, San Francisco, California, USA, 3–7 December 2012, T43E-2712, http://fallmeeting.agu.org/2012/eposters/eposter/t43e-2712/, 2012c.
Pownall, J. M., Hall, R., and Watkinson, I. M.: Granulites from the Kobipoto Mountains of Seram, eastern Indonesia, linked to extensional exhumation of mantle peridotites, Granulites & Granulites 2013, Hyderabad, India, 16–20 January 2013, 2013a.
Pownall, J. M., Hall, R., and Watkinson, I. M.: Pliocene extension on Seram and Ambon, eastern Indonesia, linked to mantle exhumation and granulite facies metamorphism, Tectonic Studies Group AGM, Leeds, UK, 3–5 January 2013, 2013b.
Pownall, J. M., Hall, R., and Watkinson, I. M.: granulite facies metamorphism and melting in the Kobipoto Mountains of Seram, eastern Indonesia, driven by mantle exhumation, Metamorphic Studies Group Research-in-Progress Meeting 2013, Cambridge, UK, 20 March 2013, 2013c.
Price, P. L.: Miospore and phytoplankton assemblages from basement samples, Seram, Indonesia, AAR Ltd., Laboratory Report No. 200/1, 1976.
Price, P. L., O'Sullivan, T., and Alexander, R.: Nature and occurence of oil in Seram, Indonesia, Proc. Indones. Petrol. Assoc., 6, 141–173, 1987.
Priem, H. N. A., Andriessen, P. A. M., Boelrijk, N. A. I. M., Hebeda, E. H., Hutchinson, C. S., Verdurmen, E. A. T., and Versschure, R. H.: Isotopic evidence for a middle to late Pliocene age of the cordierite granite on Ambon, Indonesia, Geol. Mijnbouw, 57, 441–443, 1978.
Rutten, L. M. R.: Uit het eerste verslag over de geologische expeditie naar Ceram, Tijd. K. Ned. Aardr. Gen., 35, 112–121, 1918a.
Rutten, L. M. R.: De geologische expeditie naar Ceram- tweede verslag (13 Aug.- 11 Sept. 1917), Tijd. K. Ned. Aardr. Gen., 35, 228–234, 1918b.
Rutten, L. M. R.: De geologische expeditie naar Ceram- derde verslag (12 Sept.- 11 Nov. 1917), Tijd. K. Ned. Aardr. Gen., 35, 368–378, 1918c.
Rutten, L. M. R.: De geologische expeditie naar Ceram- vierde verslag (12 Nov. 1917–4 Jan. 1918), Tijd. K. Ned. Aardr. Gen., 35, 547–555, 1918d.
Rutten, L. M. R.: De geologische expeditie naar Ceram- vijfde verslag (4 Jan.– einde Maart 1918), Tijd. K. Ned. Aardr. Gen., 36, 36–48, 1919a.
Rutten, L. M. R.: De geologische expeditie naar Ceram- zesde verslag (April – Mei 1918), Tijd. K. Ned. Aardr. Gen., 36, 1919b.
Rutten, L. M. R.: De geologische expeditie naar Ceram- sevende verslag (Juni–Juli 1918), Tijd. K. Ned. Aardr. Gen., 36, 199–207, 1919c.
Rutten, L. M. R.: De geologische expeditie naar Ceram- achtse verslag., Tijd. K. Ned. Aardr. Gen., 36, 460–466, 1919d.
Rutten, L. M. R.: Ceram, Ambon, Boeroe en de kleinere eilanden in hunne omgeving, in: Voordrachten over de geologie van Nederlandsch Indie, edited by: Rutten, L. M. R., 716–749, Wolters, Groningen, 1927.
Rutten, L. M. R. and Hotz, W.: De geologische expeditie naar Ceram- negende verslag (medio September–medio December 1918), Tijd. K. Ned. Aardr. Gen., 36, 559–579, 1919.
Rutten, L. M. R. and Hotz, W.: De geologische expeditie naar Ceram- tiende verslag (medio September–medio December 1918), Tijd. K. Ned. Aardr. Gen., 37, 17–31, 1920a.
Rutten, L. M. R. and Hotz, W.: De geologische expeditie naar Ceram- elfde (laaste) verslag (13 Aug.–11 Sept. 1917), Tijd. K. Ned. Aardr. Gen., 37, 32–42, 1920b.
Sandiford, M., Neall, F. B., and Powell, R.: Metamorphic evolution of aluminous granulites from Labwor Hills, Uganda, Contrib. Mineral. Petr., 95, 217–225, 1987.
Sawyer, E. W.: Atlas of Migmatites, vol. 9, The Canadian Mineralogist, Special Publication, Ottawa, Canada, 9 Edn., 2008.
Schroeder van der Kolk, J. L. C.: Mikroskopische Studien ueber Gesteine aus den Molukken, pt. 2 - Gesteine von Seran, Geol. Reichs-Museums Leiden, Samml., 6, 1–39, 1902.
Seidel, M., Pack, A., Sharp, Z. D., and Seidel, E.: The Kakopetros and Ravdoucha iron-oxide deposits, western Crete, Greece: fluid transport and mineralization within a detachment zone, Econ. Geol., 100, 165–174, 2005.
Sevastjanova, I., Hall, R., Gunawan, I., Ferdian, F., Decker, J.: Continental crust history in SE Asia: Insights from zircon geochronology, 2012 Fall Meeting, AGU, San Francisco, California, USA, 3–7 December 2012, T11B-2572, http://fallmeeting.agu.org/2012/eposters/eposter/t11b-2572/, 2012.
Smith, S. A. F., Holdsworth, R. E., and Collettini, C.: Interactions between low-angle normal faults and plutonism in the upper crust: Insights from the Island of Elba, Italy, Geol. Soc. Am. Bull., 123, 329–346, https://doi.org/10.1130/B30200.1, 2010.
Spakman, W. and Hall, R.: Surface deformation and slab–mantle interaction during Banda arc subduction rollback, Nat. Geosci., 3, 562–566, https://doi.org/10.1038/ngeo917, 2010.
Špičák, A., Matějková, R., and Vaněk, J.: Seismic response to recent tectonic processes in the Banda Arc region, J. Asian Earth Sci., 64, 1–13, https://doi.org/10.1016/j.jseaes.2012.11.014, 2013.
Stevens, C. W., McCaffrey, R., Bock, Y., Genrich, J. F., Pubellier, M., and Subarya, C.: Evidence for Block Rotations and Basal Shear in the World's Fastest Slipping Continental Shear Zone in NW New Guinea, in: Plate Boundary Zones, edited by: Stein, S. and Freymueller, J., AGU Geodynam. Ser., 30, 87–99, 2002.
Teas, P. A., Decker, J., Orange, D., and Baillie, P.: New insight into the structure and tectonics of the Seram Trough from SEASTEEP high resolution bathymetry, Proc. Indones. Petrol. Assoc., 33, 2009.
Tjokrosapoetro, S.: The regional structures of Seram Island as interpreted from satellite imagery, Geological Research and Development Centre, Bandung, Indonesia, 1976.
Tjokrosapoetro, S. and Budhitrisna, T.: Geology and tectonics of the northern Banda Arc, B. Indones. Geol. Res. Dev. Cent., 6, 1–17, 1982.
Tjokrosapoetro, S., Rusmana, E., Sukardi, and Achdan, A.: Preliminary geological map of the Ambon Quadrangle, Maluku. Scale 1:250,000, Geological Research and Development Centre, Bandung, Indonesia,1985.
Tjokrosapoetro, S., Achdan, A., Suwitodirdjo, K., and Abidin: Preliminary geological map of the Masohi Quadrangle, Maluku. Scale 1:250,000, Geological Research and Development Centre, Bandung, Indonesia, 1987.
Tjokrosapoetro, S., Achdan, A., Suwitodirdjo, K., Rusmana, E., and Abidin, H. Z.: Geological map of the Masohi quadrangle, Maluku, 1:250000, Geological Research and Development Centre, Bandung, Indonesia, 1993a.
Tjokrosapoetro, S., Rusmana, E., and Achdan, A.: Geological map of the Ambon sheet, Maluku, 1:250,000, Geological Research and Development Centre, Bandung, Indonesia, 1993b.
Tsunogae, T. and Santosh, M.: Spinel–sapphirine–quartz bearing composite inclusion within garnet from an ultrahigh-temperature pelitic granulite: Implications for metamorphic history and P-T path, Lithos, 92, 524–536, https://doi.org/10.1016/j.lithos.2006.03.060, 2006.
Valk, W.: Contributions to the geology of West Seran, in: Geological, petrographical, and palaeontological results of explorations, carried out from September 1917 till June 1919 in the island of Ceram, edited by: Rutten, L. and Hotz, W., De Bussy, Amsterdam, 1, 104 pp., 1945.
van Bemmelen, R. W.: The geology of Indonesia, Government Printing Office, Matinus Nijhoff, The Hague, 1949.
van Bergen, M. J., Erfan, R. D., Sriwana, T., Suharyono, K., Poorter, R. P. E., Varekamp, J. C., Vroon, P. Z., and Wirakusumah, A. D.: Spatial geochemical variations of arc volcanism around the Banda Sea, Neth. J. Sea Res., 24, 313–322, 1989.
van der Sluis, J. P.: Geology of East Seran, in: Geological, petrographical, and palaeontological results of explorations, carried out from September 1917 till June 1919 in the island of Ceram, edited by: Rutten, L. and Hotz, W., De Bussy, Amsterdam, 3, 67 pp., 1950.
van Hinte, J. E. and Hartono, H. M. S.: Executive summary of Theme I Snellius-II Expedition "Geology and geophysics of the Banda Arc and adjacent areas", Neth. J. Sea Res., 24, 95–102, 1989.
Verbeek, R. D. M.: Geologische beschrijving van Ambon, Jaarb. Mijnw. Ned. Oost-Indie, 29, 308, 1905.
Villeneuve, M., Martini, R., Bellon, H., Réhault, J.-P., Cornée, J.-J., Bellier, O., Burhannuddin, S., Hinschberger, F., Honthaas, C., and Monnier, C.: Deciphering of six blocks of Gondwanan origin within Eastern Indonesia (South East Asia), Gondwana Res., 18, 420–437, https://doi.org/10.1016/j.gr.2009.12.011, 2010.
Visser, W. A. and Hermes, J. J.: Geological results of the exploration for oil in Netherlands New Guinea, Verhandelingen Koninklijk Nederlands Geologisch en Mijnbouwkundig Genootschap, 20, 265, 1962.
Vroon, P., Lowry, D., Van Bergen, M. J., Boyce, A. J., and Mattey, D. P.: Oxygen isotope systematics of the Banda Arc: low δ18O despite involvement of subducted continental material in magma genesis, Geochim. Cosmochim. Ac., 65, 589–609, https://doi.org/10.1016/S0016-7037(00)00554-8, 2001.
Walker, J. D. and Geissman, J. W.: 2009 Geological Time Scale, Geol. Soc. Am., https://doi.org/10.1130/2009.CTS004R2C, 2009.
Wanner, J.: Triaspetrefakten der Molukken und des Timorarchipels, Neues Jahrbuch Min., Geol., Palaont., Beilage Band, 24, 133–160, 1907.
Wanner, J.: Geologische Ergebnisse der Reisen K. Deninger's in den Molukken. I. Beitrage zur Geologie der Insel Buru, Palaeontographica, Suppl. IV, Beitr. Geologie Niederlandisch-Inden III, 3, 59–112, 1923.
Waters, D. J.: Hercynite–quartz granulites: phase relations and implications for crustal processes, Eur. J. Mineral., 3, 367–386, 1991.
Watkinson, I. M., Hall, R., Cottam, M. A., Sevastjanova, I., Suggate, S., Gunawan, I., Pownall, J. M., Hennig, J., Ferdian, F., Gold, D., Zimmermann, S., Rudyawan, A., and Advocaat, E.: New Insights Into the Geological Evolution of Eastern Indonesia From Recent Research Projects by the SE Asia Research Group, Berita Sedimentol., 23, 21–27, 2012.
Whitford, D. J. and Jezek, P. A.: Origin of late Cenozoic lavas from the Banda Arc, Indonesia: trace elements and Sr isotope evidence, Contrib. Mineral. Petr., 68, 141–150, 1979.
Whitney, D. L., Teyssier, C., Rey, P., and Buck, W. R.: Continental and oceanic core complexes, Geol. Soc. Am. Bull., 125, 273–298, https://doi.org/10.1130/B30754.1, 2013.
Widiyantoro, S. and van der Hilst, R.: Mantle structure beneath Indonesia inferred from high-resolution tomographic imaging, Geophys. J. Int., 130, 167–182, 1997.
Widiyantoro, S., Pesicek, J. D., and Thurber, C. H.: Complex structure of the lithospheric slab beneath the Banda arc, eastern Indonesia depicted by a seismic tomographic model, Res. Geophys., 1, 1–6, https://doi.org/10.4081/rg.2011.e1, 2011.
Zeck, H. P.: An erupted migmatite from Cerro del Hoyazo, SE Spain, Contrib. Mineral. Petr., 26, 225–246, 1970.
Zeck, H. P. and Williams, I. S.: Inherited and magmatic zircon from neogene Hoyazo cordierite dacite, SE Spain – Anatectic source rock provenance and magmatic evolution, J. Petrol., 43, 1089–1104, 2002.
Zillman, N. J. and Paten, R. J.: Exploration and petroleum prospects, Bula Basin, Seram, Indonesia, Proc. Indones. Petrol. Assoc., 4, 129–148, 1975.