Lower Cretaceous Provenance and Sedimentary Deposition in the Eastern Carpathians: Inferences for the Evolution of the Subducted Oceanic Domain and its European Passive Continental Margin

Author:

Roban R. D.1ORCID,Ducea M. N.12ORCID,Mațenco L.3ORCID,Panaiotu G. C.4ORCID,Profeta L.12,Krézsek C.5,Melinte‐Dobrinescu M. C.6,Anastasiu N.1ORCID,Dimofte D.1,Apotrosoaei V.1,Francovschi I.1

Affiliation:

1. Faculty of Geology and Geophysics University of Bucharest Bucharest Romania

2. Department of Geosciences University of Arizona Tucson AZ USA

3. Faculty of Geosciences Utrecht University Utrecht Netherlands

4. Faculty of Physics University of Bucharest Bucharest Romania

5. OMV Petrom Bucharest Romania

6. National Institute of Marine Geology and Geo‐Ecology Bucharest Romania

Funder

Unitatea Executiva pentru Finantarea Invatamantului Superior, a Cercetarii, Dezvoltarii si Inovarii

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference153 articles.

1. What are the “Green clasts” of the Carpathian flysch? A petrographic reconsideration;Anastasiu N.;Revue Roumaine de Géologie Géophysique et Géographie, Academia Română,1984

2. Tectono-thermal regimes and lithosphere behaviour in the External Dacides in the Upper Triassic and Jurassic Tethyan opening (Romanian Carpathians)

3. Symmetry during the syn- and post-rift evolution of extensional back-arc basins: The role of inherited orogenic structures

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