The effect of the faults to the tectono-stratigraphy evolution in the Panyu low uplift

Introduction: The Panyu low uplift is located in the middle of the Central Uplift Belt of the Pearl River Mouth Basin, which has experienced multiple episodes of tectonic movements since the Cenozoic, and the faults are extensively developed there. The fault activities had a significant influence on...

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Egile Nagusiak:	Yuanyuan Liang, Dongsheng Yang, Shi Chen, Gongcheng Zhang, Zhizhao Bai, Xinxin Liang, Yunuo Wang, Long Wang, Shuai Guo, Mo Ji, Hui Yan
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Frontiers Media S.A. 2024-01-01
Saila:	Frontiers in Earth Science
Gaiak:	residual depression tension-shear fault tectonic evolution Panyu low uplift Pearl River Mouth Basin sedimentary filling
Sarrera elektronikoa:	https://www.frontiersin.org/articles/10.3389/feart.2023.1281153/full
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