Evolution of a mixed siliciclastic‐carbonate deep‐marine system on an unstable margin: The Cretaceous of the Eastern Greater Caucasus, Azerbaijan-Reference-Cited by-同舟云学术

Evolution of a mixed siliciclastic‐carbonate deep‐marine system on an unstable margin: The Cretaceous of the Eastern Greater Caucasus, Azerbaijan

Published:2020-08-11 Issue:1 Volume:33 Page:612-647
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Res

Author:

Cumberpatch Zoë A.¹^ORCID,Soutter Euan L.¹^ORCID,Kane Ian A.¹^ORCID,Casson Max¹^ORCID,Vincent Stephen J.²^ORCID

Affiliation:

1. Department of Earth and Environmental Sciences University of Manchester Manchester UK

2. CASP Cambridge UK

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12488

Reference169 articles.

1. Geology of the Caucasus: A review;Adamia S. A.;Turkish Journal of Earth Sciences,2011

2. Geosciences of Azerbaijan

3. Anatomy of carbonate breccias, turbidite facies and depositional systems of Gercus Formation, in Donkan Area, Northern Iraq;Al‐Mashaikie S. Z. A. K.;Iraqi Geological Journal,2017

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