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Volume 7, issue 1
Solid Earth, 7, 11–36, 2016
https://doi.org/10.5194/se-7-11-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: From orogenesis to geoscience in the service of society: the...

Solid Earth, 7, 11–36, 2016
https://doi.org/10.5194/se-7-11-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 15 Jan 2016

Research article | 15 Jan 2016

The Imbert Formation of northern Hispaniola: a tectono-sedimentary record of arc–continent collision and ophiolite emplacement in the northern Caribbean subduction–accretionary prism

J. Escuder-Viruete et al.
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Cited articles  
Abbott, R. N. and Draper, G.: The Case for UHP Conditions in the Cuaba Terrane, Rio San Juan Metamorphic Complex, Dominican Republic, Geol. Ac., 11, 149–165, 2013.
Agard, P., Yamato, P., Jolivet, L., and Burov, E.: Exhumation of oceanic blueschists and eclogites in subduction zones: Timing and mechanisms, Earth Sci. Rev., 92, 53–79, 2009.
Alonso, J. L., Marcos, A., and Suárez, A.: Structure and organization of the Porma mélange: Progressive denudation of a submarine nappe toe by gravitational collapse, Am. J. Sci., 306, 32–65 2006.
Alonso, J. L., Marcos, A., Villa, E., Súarez, A., Merino-Tomé, O. A., and Fernández, L. P.: Mélanges and other types of block-in-matrix formations in the Cantabrian Zone (Variscan Orogen, northwest Spain): origin and significance, Int. Geol. Rev., 57, 563–580, 2015.
Bourgois, J., Vila, J. M., Llinás, R., and Tavares, I.: Datos geológicos nuevos acerca de la región de Puerto Plata, República Dominicana, Transactions of the 9th Caribbean Geological Conference, Republica Dominicana, Amigo del Hogar Publishers, Santo Domingo, 35–38, 1982.
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Short summary
New stratigraphical, structural, geochemical, and geochronological data from the northern Caribbean orogenic belt indicate that the Imbert Fm constitutes a coarsening-upward stratigraphic sequence that records the transition of the sedimentation from a pre-collisional forearc to a syn-collisional piggy-back basin in the lower-to-middle Eocene. This piggy-back basin was transported to the top of the Puerto Plata ophiolitic slab as it was emplaced onto the North America continental margin units.
New stratigraphical, structural, geochemical, and geochronological data from the northern...
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