Extensional and transtensional tectonic deformation leads to the formation of fault-bounded sedimentary basins, which may be inverted by subsequent compressional or transpressional tectonic events. Examples of such inverted basins can be found around the globe, and an in-depth understanding of inversion processes is not only important from a scientific – structural geology and tectonics – point of view but also for unravelling trap structures that can play a role in resource exploration and underground storage. Analogue modellers have studied basin inversion processes since at least the 1980s, providing important insights into the dynamics involved, but have dedicated only limited attention to the topic over the past decade(s). This special issue therefore aims to spark a renewal of basin inversion modelling efforts, and we invite contributions focussing on a number of suggested key topics (see below).

Next to advancing fundamental concepts in basin inversion through cutting-edge analogue modelling efforts, this special issue is also intended to promote and further establish analogue modelling as a quantitative method for studying tectonic processes and to bring together the international analogue modelling community (with full support from the EPOS Multi-scale Laboratories, MSL, network). We therefore urge authors not only to present novel modelling studies of basin inversion but also to actively discuss, establish, modernize and describe (lab) protocols and to include extensive background information on their modelling techniques. We furthermore encourage creating videos or poster presentations that can be shared online, broadcasting the magic and beauty of analogue modelling to the wider (Earth sciences) community and to the general public.

Recent advances in acquisition design and fibre composition have led to an increasing number of fibre-optic sensing applications for both distributed and point sensor systems. In Earth sciences, these fibre-optic technologies are used to sample strain, temperature or chemicals in a great variety of environments such as boreholes, deep seas, at the surface and also in densely populated areas. In recent years, we have observed an explosion of pilot experiments leading to new applications and technological breakthroughs in many fields of Earth sciences.

The aim of this special issue is to gather and highlight different techniques, methods and applications these fibre-optic technologies offer to Earth sciences and to provide a broad perspective on recent and further developments (technical, numerical and methodological) in these new research fields. Contributions from all areas of applied geosciences (geochemistry, geophysics, geodesy, natural hazards, oceanography, soil science, geo-energy, civil and environmental engineering, volcanology, hydrology, glaciology, and many others) using fibre-optical cable sensing are welcome. We encourage including qualitative and quantitative case studies, embracing laboratory studies, large-scale field tests and modelling.

This special issue looks at inversion tectonics 3 decades after a late 1980s peak in interest that is documented, for instance, by a 1987 Tectonophysics special issue and a 1989 Geol. Soc. London book that soon became classics. Today inversion tectonics is well established as a basic concept, but by far not all aspects of it are well understood. Even the enormous variety of associated structures has probably not been exhaustively described and explained. The kinematics of inversion structures is particularly complex, and their mechanics a matter of debate. The special issue is meant to illustrate the advances made over the past 30 years but also to point out open questions. It has its roots in a session on inversion tectonics at the 2019 EGU General Assembly. Announced contributions already cover many aspects including the importance of inversion concepts in petroleum exploration, the role of plate-wide stress changes and plate rigidity, improved kinematic and timing constraints for well-studied examples, inversion interfering with regional uplift, and inversion of salt-bearing basins. Case studies, often based on high-resolution seismic data, cover diverse areas from Australia to Scandinavia and inversion events from the Paleoproterozoic to the Paleogene. We invite additional contributions dealing with all aspects of inversion tectonics from architecture over kinematics to dynamics and from field- or seismics-based case studies to analogue and numerical simulations, also including responses of depositional systems to active inversion tectonics. The focus will be on "positive inversion", i.e. a change from normal faulting to thrusting or transpression. However, papers on other cases of fault reactivation would also fit our envisaged frame. We particularly welcome new hypotheses challenging common wisdom!

The special issue is dedicated to state-of-the art research on the Alps and the adjacent orogens. It will improve our understanding of mountain-building processes and the past and ongoing tectonic evolution in the region. This multi- and interdisciplinary effort integrates geophysics, tectonics, petrology, geochronology, and basin and surface studies. The contributions highlight recent efforts to image deep structures, track motion and deformation of the crust and mantle through time, and investigate the surface response to deep-seated processes. Thus, the volume will highlight recent results from the European AlpArray project, which has featured an unprecedentedly dense seismic station network in the Alpine region. We invite researchers from inside and outside the AlpArray project and from all fields to contribute to this volume.

This issue is derived from the EGU Sharing Geosciences Online 2020’s session ERE5.4, entitled “State-of-the-art in mineral exploration”. The rationale behind this proposal is to bring together a number of articles aimed at exploring the current state and future prospects of mineral exploration, from different perspectives (e.g. remote sensing, geochemistry, geology, geophysics, modelling, mineralogy, structural geology).

Mineral resources are used in larger quantities than ever before in history, and are the basis of our modern society. The safe and sustainable supply of mineral resources is fostering a demand for innovative actions to cover the foreseeable future industry and human demands. Exploration is the first step in the mineral resources cycle. On the one hand, most of the giant deposits at shallow depths have been already explored and mined out and the industry is moving towards deeper and more complex mineral systems, which brings significant exploration challenges. On the other hand, the exploration sector needs time-saving, cost-effective, and, particularly in Europe, environmentally friendly and socially acceptable techniques to ensure sustainable access to mineral resources.

This special issue aims to bring together a meaningful collection of articles that will shape the mineral exploration for the 21st century. Articles can include, but are not limited to, the following topics: new methods of exploration; imaging; conceptual modelling and quantification of deposits and mineral systems; cost reduction in exploration; non-invasive exploration; environmentally sustainable exploration; integration of multidisciplinary methodologies and datasets; scale-up and replicability; industry–academia synergies; and FAIR data repositories.

The special issue arises out of an international workshop on “Tools, data and models for 3D seismotectonics: the Italian laboratory over time” that was held in Perugia on 9–10 July 2019. The workshop was organized by the Inter-University CENTRE for 3D Seismotectonics (CRUST, Italy) to commemorate Professor Giampaolo Pialli, who died suddenly 20 years ago, at the age of 59. Giampaolo was an open-minded and inclusive researcher of the University of Perugia, especially keen on the use of multidisciplinary and multi-scale approaches in active and sustained geological processes of deformation. The main aim of the workshop was to promote new research and interdisciplinary collaborations among structural geologists and geophysicists who operate in the field of seismotectonics, at local and regional scales, with the common goal to reach a deep understanding of earthquake–fault interactions and to build realistic 3-D structural–seismotectonic fault models for better evaluation of seismic hazards with consequent seismic risk reduction.

This special issue has the purpose of collecting high-quality papers presented at the workshop but is not restricted to these. The main goal is to put together a reference volume that contains the most innovative and as complete as possible knowledge on Italian seismotectonics and seismogenesis, analysed at various spatial and temporal scales and taken as a methodological example for multidisciplinary and interdisciplinary studies in other areas of high seismic hazard.

The main topics of interest include

• observational seismology for seismotectonics and earthquake mechanics;
• active tectonics and surface faulting;
• geophysical data and modelling for seismotectonics;
• 3-D geometric–kinematic and dynamic active and evolutionary fault models.

This joint special issue between Solid Earth and Geoscience Communication aims to present the highlights of recent efforts of a global community of educators and researchers to develop virtual field activities to enhance student learning, research, and broader outreach. These resilient, non-traditional solutions to field-focused investigations ensure that students achieve intended learning outcomes and curricular requirements even when physical contact and travel are restricted. The special issue will ensure that the virtual field experiences initially developed as short-term solutions to the COVID-19 pandemic will become valuable longer-term resources that will increase the accessibility of field experiences for students and society.

We invite contributions that describe, discuss, and evaluate aspects of virtual field experiences, trips, and exercises, including but not limited to

• intended learning outcomes,
• methods employed in exercise design and construction,
• outreach and communication with wider society,
• how the field excursion enhances relevant previous research on the topic or location.

We have made special provisions to publish supplementary datasets that could include

• photographs, videos, and 3D models,
• geographical annotation files, such as Google Earth presentations and/or KML/KMZ files or ESRI shapefiles,
• educational materials, such as exercise descriptions, rubrics, background literature, etc.,
• links to datasets hosted in external repositories, preferably via a DOI, but if necessary as hyperlinks to material hosted on websites, such as the NAGT Teaching with Online Field Experiences site and V3Geo 3D models.

If you have other ideas, please do not hesitate to contact the special issue editors prior to submission to discuss whether they can be included.

Volcanology has made great advances in the last 3 decades, becoming a modern interdisciplinary science that has learned how to quantify volcanic processes, their associated hazards and resources, as well as the impact of volcanic activity on society and the environment. Numerical models are developed in order to better understand volcanic processes and aid in hazard prediction. At the same time, an accurate forecasting of future volcanic events requires detailed understanding of past trends. Because models can describe only a simplified version of complex natural processes, geologic and field data are critical for constraining model input, necessary for model validation, and will ultimately improve model accuracy. The aim of this special issue is to present studies in which traditional field-based methods are conceived and used for constraining, improving, and validating numerical models describing volcanic processes. We collect contributions describing field data and the role of volcano geology in model validation for a wide range of volcanic phenomena, including tephra fall, pyroclastic density currents, and lava flows. The contributions listed below arise out of both an IAVCEI COV10 session in 2018 and an open call for contributions. The volume is under aegis of IAVCEI Volcano Geology commission.

Extensional and transtensional tectonic deformation leads to the formation of fault-bounded sedimentary basins, which may be inverted by subsequent compressional or transpressional tectonic events. Examples of such inverted basins can be found around the globe, and an in-depth understanding of inversion processes is not only important from a scientific – structural geology and tectonics – point of view but also for unravelling trap structures that can play a role in resource exploration and underground storage. Analogue modellers have studied basin inversion processes since at least the 1980s, providing important insights into the dynamics involved, but have dedicated only limited attention to the topic over the past decade(s). This special issue therefore aims to spark a renewal of basin inversion modelling efforts, and we invite contributions focussing on a number of suggested key topics (see below).

Next to advancing fundamental concepts in basin inversion through cutting-edge analogue modelling efforts, this special issue is also intended to promote and further establish analogue modelling as a quantitative method for studying tectonic processes and to bring together the international analogue modelling community (with full support from the EPOS Multi-scale Laboratories, MSL, network). We therefore urge authors not only to present novel modelling studies of basin inversion but also to actively discuss, establish, modernize and describe (lab) protocols and to include extensive background information on their modelling techniques. We furthermore encourage creating videos or poster presentations that can be shared online, broadcasting the magic and beauty of analogue modelling to the wider (Earth sciences) community and to the general public.

This joint special issue between Solid Earth and Geoscience Communication aims to present the highlights of recent efforts of a global community of educators and researchers to develop virtual field activities to enhance student learning, research, and broader outreach. These resilient, non-traditional solutions to field-focused investigations ensure that students achieve intended learning outcomes and curricular requirements even when physical contact and travel are restricted. The special issue will ensure that the virtual field experiences initially developed as short-term solutions to the COVID-19 pandemic will become valuable longer-term resources that will increase the accessibility of field experiences for students and society.

We invite contributions that describe, discuss, and evaluate aspects of virtual field experiences, trips, and exercises, including but not limited to

• intended learning outcomes,
• methods employed in exercise design and construction,
• outreach and communication with wider society,
• how the field excursion enhances relevant previous research on the topic or location.

We have made special provisions to publish supplementary datasets that could include

• photographs, videos, and 3D models,
• geographical annotation files, such as Google Earth presentations and/or KML/KMZ files or ESRI shapefiles,
• educational materials, such as exercise descriptions, rubrics, background literature, etc.,
• links to datasets hosted in external repositories, preferably via a DOI, but if necessary as hyperlinks to material hosted on websites, such as the NAGT Teaching with Online Field Experiences site and V3Geo 3D models.

If you have other ideas, please do not hesitate to contact the special issue editors prior to submission to discuss whether they can be included.

This issue is derived from the EGU Sharing Geosciences Online 2020’s session ERE5.4, entitled “State-of-the-art in mineral exploration”. The rationale behind this proposal is to bring together a number of articles aimed at exploring the current state and future prospects of mineral exploration, from different perspectives (e.g. remote sensing, geochemistry, geology, geophysics, modelling, mineralogy, structural geology).

Mineral resources are used in larger quantities than ever before in history, and are the basis of our modern society. The safe and sustainable supply of mineral resources is fostering a demand for innovative actions to cover the foreseeable future industry and human demands. Exploration is the first step in the mineral resources cycle. On the one hand, most of the giant deposits at shallow depths have been already explored and mined out and the industry is moving towards deeper and more complex mineral systems, which brings significant exploration challenges. On the other hand, the exploration sector needs time-saving, cost-effective, and, particularly in Europe, environmentally friendly and socially acceptable techniques to ensure sustainable access to mineral resources.

This special issue aims to bring together a meaningful collection of articles that will shape the mineral exploration for the 21st century. Articles can include, but are not limited to, the following topics: new methods of exploration; imaging; conceptual modelling and quantification of deposits and mineral systems; cost reduction in exploration; non-invasive exploration; environmentally sustainable exploration; integration of multidisciplinary methodologies and datasets; scale-up and replicability; industry–academia synergies; and FAIR data repositories.

The special issue is dedicated to state-of-the art research on the Alps and the adjacent orogens. It will improve our understanding of mountain-building processes and the past and ongoing tectonic evolution in the region. This multi- and interdisciplinary effort integrates geophysics, tectonics, petrology, geochronology, and basin and surface studies. The contributions highlight recent efforts to image deep structures, track motion and deformation of the crust and mantle through time, and investigate the surface response to deep-seated processes. Thus, the volume will highlight recent results from the European AlpArray project, which has featured an unprecedentedly dense seismic station network in the Alpine region. We invite researchers from inside and outside the AlpArray project and from all fields to contribute to this volume.

Recent advances in acquisition design and fibre composition have led to an increasing number of fibre-optic sensing applications for both distributed and point sensor systems. In Earth sciences, these fibre-optic technologies are used to sample strain, temperature or chemicals in a great variety of environments such as boreholes, deep seas, at the surface and also in densely populated areas. In recent years, we have observed an explosion of pilot experiments leading to new applications and technological breakthroughs in many fields of Earth sciences.

The aim of this special issue is to gather and highlight different techniques, methods and applications these fibre-optic technologies offer to Earth sciences and to provide a broad perspective on recent and further developments (technical, numerical and methodological) in these new research fields. Contributions from all areas of applied geosciences (geochemistry, geophysics, geodesy, natural hazards, oceanography, soil science, geo-energy, civil and environmental engineering, volcanology, hydrology, glaciology, and many others) using fibre-optical cable sensing are welcome. We encourage including qualitative and quantitative case studies, embracing laboratory studies, large-scale field tests and modelling.

Volcanology has made great advances in the last 3 decades, becoming a modern interdisciplinary science that has learned how to quantify volcanic processes, their associated hazards and resources, as well as the impact of volcanic activity on society and the environment. Numerical models are developed in order to better understand volcanic processes and aid in hazard prediction. At the same time, an accurate forecasting of future volcanic events requires detailed understanding of past trends. Because models can describe only a simplified version of complex natural processes, geologic and field data are critical for constraining model input, necessary for model validation, and will ultimately improve model accuracy. The aim of this special issue is to present studies in which traditional field-based methods are conceived and used for constraining, improving, and validating numerical models describing volcanic processes. We collect contributions describing field data and the role of volcano geology in model validation for a wide range of volcanic phenomena, including tephra fall, pyroclastic density currents, and lava flows. The contributions listed below arise out of both an IAVCEI COV10 session in 2018 and an open call for contributions. The volume is under aegis of IAVCEI Volcano Geology commission.

The special issue arises out of an international workshop on “Tools, data and models for 3D seismotectonics: the Italian laboratory over time” that was held in Perugia on 9–10 July 2019. The workshop was organized by the Inter-University CENTRE for 3D Seismotectonics (CRUST, Italy) to commemorate Professor Giampaolo Pialli, who died suddenly 20 years ago, at the age of 59. Giampaolo was an open-minded and inclusive researcher of the University of Perugia, especially keen on the use of multidisciplinary and multi-scale approaches in active and sustained geological processes of deformation. The main aim of the workshop was to promote new research and interdisciplinary collaborations among structural geologists and geophysicists who operate in the field of seismotectonics, at local and regional scales, with the common goal to reach a deep understanding of earthquake–fault interactions and to build realistic 3-D structural–seismotectonic fault models for better evaluation of seismic hazards with consequent seismic risk reduction.

This special issue has the purpose of collecting high-quality papers presented at the workshop but is not restricted to these. The main goal is to put together a reference volume that contains the most innovative and as complete as possible knowledge on Italian seismotectonics and seismogenesis, analysed at various spatial and temporal scales and taken as a methodological example for multidisciplinary and interdisciplinary studies in other areas of high seismic hazard.

The main topics of interest include

• observational seismology for seismotectonics and earthquake mechanics;
• active tectonics and surface faulting;
• geophysical data and modelling for seismotectonics;
• 3-D geometric–kinematic and dynamic active and evolutionary fault models.

This special issue looks at inversion tectonics 3 decades after a late 1980s peak in interest that is documented, for instance, by a 1987 Tectonophysics special issue and a 1989 Geol. Soc. London book that soon became classics. Today inversion tectonics is well established as a basic concept, but by far not all aspects of it are well understood. Even the enormous variety of associated structures has probably not been exhaustively described and explained. The kinematics of inversion structures is particularly complex, and their mechanics a matter of debate. The special issue is meant to illustrate the advances made over the past 30 years but also to point out open questions. It has its roots in a session on inversion tectonics at the 2019 EGU General Assembly. Announced contributions already cover many aspects including the importance of inversion concepts in petroleum exploration, the role of plate-wide stress changes and plate rigidity, improved kinematic and timing constraints for well-studied examples, inversion interfering with regional uplift, and inversion of salt-bearing basins. Case studies, often based on high-resolution seismic data, cover diverse areas from Australia to Scandinavia and inversion events from the Paleoproterozoic to the Paleogene. We invite additional contributions dealing with all aspects of inversion tectonics from architecture over kinematics to dynamics and from field- or seismics-based case studies to analogue and numerical simulations, also including responses of depositional systems to active inversion tectonics. The focus will be on "positive inversion", i.e. a change from normal faulting to thrusting or transpression. However, papers on other cases of fault reactivation would also fit our envisaged frame. We particularly welcome new hypotheses challenging common wisdom!