Depositional evolution and models for a deep-lacustrine gravity flow system in a half-graben rifted sag, Beibuwan Basin, South China Sea

Depositional evolution and models for a deep-lacustrine gravity flow system in a half-graben rifted sag, Beibuwan Basin, South China Sea

The Paleogene Liushagang Formation is part of the Fushan Sag, a continental lacustrine basin located at the Southeastern margin of the Beibuwan Basin, South China Sea. Further understanding of the deep-water gravity flow deposits in this formation will be conducive to lithologic reservoir exploratio...

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Bibliographic Details
Main Authors: Yuan Li, Hua Wang, Jie Qiong Zhu, Guo Tao Zhang, Hao Guo, Xiao Han Li, Song Lin, Jin Min
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2022-03-01
Series:Geologica Acta
Subjects:
deep-lacustrine gravity flow
turbidity current
sandy debrite
fushan sag
beibuwan basin
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/33070/37454

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https://revistes.ub.edu/index.php/GEOACTA/article/view/33070/37454

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