Initiation and evolution of fault‐controlled slope‐parallel submarine channels: Miocene eastern slope of Yinggehai Basin, South China Sea-Reference-Cited by-同舟云学术

Initiation and evolution of fault‐controlled slope‐parallel submarine channels: Miocene eastern slope of Yinggehai Basin, South China Sea

Published:2022-10-26 Issue:2 Volume:35 Page:592-619
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Research

Author:

Wang Zhen¹²³,Xian Benzhong²⁴,Liu Jingyan¹,Khan Majid⁵^ORCID,Fan Caiwei⁶,Li Hui⁶,Wang Junhui²⁴^ORCID,Zhang Ximeng⁷,Liu Jianping⁸,Chen Peng²,Wu Qianran²,Zhang Wenmiao²

Affiliation:

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

2. College of Geosciences China University of Petroleum Beijing China

3. PetroChina Jidong Oilfield Company Tangshan China

4. State Key Laboratory of Petroleum Resources and Prospecting Beijing China

5. School of Civil and Resource Engineering University of Science and Technology Beijing Beijing China

6. Zhanjiang Branch of China National Offshore Oil Corporation Zhanjiang China

7. PetroChina Huabei Oilfield Company Renqiu China

8. School of Petroleum Engineering Chongqing University of Science and Technology Chongqing China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/bre.12724

Reference92 articles.

1. Morphology and distribution of Oligocene and Miocene pockmarks in the Danish North Sea - implications for bottom current activity and fluid migration

2. Morphology, seismic characteristics and development of Cap Timiris Canyon, offshore Mauritania: A newly discovered canyon preserved-off a major arid climatic region

3. Geometry and kinematics of Neogene allochthonous salt systems in the Mississippi Canyon, Atwater Valley, western Lloyd Ridge, and western DeSoto Canyon protraction areas, northern deep-water Gulf of Mexico

4. Provenance of Upper Miocene sediments in the Yinggehai and Qiongdongnan basins, northwestern South China Sea: Evidence from REE, heavy minerals and zircon U–Pb ages

5. Depositional characteristics and processes of alongslope currents related to a seamount on the northwestern margin of the Northwest Sub-Basin, South China Sea

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