Architecture and depositional processes of a submarine channel during the late Miocene in the Yinggehai basin, northwestern South China Sea-Reference-Cited by-同舟云学术

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Architecture and depositional processes of a submarine channel during the late Miocene in the Yinggehai basin, northwestern South China Sea

Published:2024-09 Issue: Volume:167 Page:106964
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Tian Dongmei^ORCID,Liang Chao,Jiang Tao,Pei Jianxiang,Liao Jin

Publisher

Elsevier BV

Reference63 articles.

1. Lateral accretion packages (LAPs): an important reservoir element in deep water sinuous channels;Abreu;Mar. Petrol. Geol.,2003

2. Latitudinal changes in submarine channel-levee system evolution, architecture and flow processes;Allen;Front. Earth Sci.,2022

3. The influence of bend amplitude and planform morphology on flow and sedimentation in submarine channels;Amos;Mar. Petrol. Geol.,2010

4. Laterally accreting sinuous channels and their deposits: the Goldilocks of deep-water slope systems;Arnott;J. Sediment. Res.,2021

5. A general model for the helical structure of geophysical flows in channel bends;Azpiroz-Zabala;Geophys. Res. Lett.,2017

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