The Late Cretaceous—Miocene supra‐salt structures in Block M, Lower Congo Basin (Congo, West Africa) and the controls on channel development-Reference-Cited by-同舟云学术

The Late Cretaceous—Miocene supra‐salt structures in Block M, Lower Congo Basin (Congo, West Africa) and the controls on channel development

Published:2022-07-12 Issue:10 Volume:57 Page:4167-4182
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Liang Chen¹²^ORCID,Ding Wenlong¹²,Liu Yaming³,Li Mingzhu¹²

Affiliation:

1. School of Energy Resources China University of Geosciences Beijing China

2. Key Laboratory for Marine Reservoir Evolution and Hydrocarbon Abundance Mechanism, Ministry of Education China University of Geosciences Beijing China

3. Research Institute of Petroleum Exploration and Development Beijing China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4536

Reference38 articles.

1. Evidence of a large upper-Cretaceous depocentre across the Continent-Ocean boundary of the Congo-Angola basin. Implications for palaeo-drainage and potential ultra-deep source rocks

2. Relating petroleum system and play development to basin evolution: West African South Atlantic basins

3. Salt tectonics at passive margins: Geology versus models

4. The development characteristics of deep water channel and sedimentary reservoir prediction in Lower Congo Basin;Cai L. L.;China Offshore Oil and Gas,2016

5. Interactions between Submarine Channels and Salt Structures: Examples from the Lower Congo Basin;Chen L.;Acta Sedimentologica Sinica,2017

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