Evolution of Sedimentary Facies of the Ordovician-Silurian Transition and Its Response to the Guangxi Movement in Southern Sichuan Basin, China

Evolution of Sedimentary Facies of the Ordovician-Silurian Transition and Its Response to the Guangxi Movement in Southern Sichuan Basin, China

The formation and distribution of sedimentary facies of the Wufeng Formation reflect the evolution of Guangxi Movement and significantly impact shale reservoir quality in southern Sichuan Basin, China. This study characterizes the sedimentary facies and their evolution of Ordovician-Silurian transit...

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Bibliographic Details
Main Authors: Guoyou Fu, Zhensheng Shi, Meng Zhao, Qun Zhao, Tianqi Zhou, Ling Qi, Pengfei Wang
Format: Article
Language:English
Published: MDPI AG 2025-03-01
Series:Applied Sciences
Subjects:
fine-grained turbidite deposits
hemipelagic deposits
shelf shoal deposits
Ordovician-Silurian (O-S) transition
Guangxi Movement
Online Access:https://www.mdpi.com/2076-3417/15/7/3559
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