Analysis of the mechanism of faulting and uplift in the Huizhou depression, Pearl River Delta, South China

机译：珠江三角洲惠州zhou陷的断层隆升机理分析

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The Huizhou depression of the Pearl River Delta is located at the junction of the Pacific, Eurasian and Indian plates.It was formed originally in the Paleogene as a continental rift basin superimposed on a setting characterized by shear stress.The formation and evolution of the basin were complex, making this feature different from a typical rift basin.

机译：珠江三角洲的惠州洼地位于太平洋，欧亚大陆和印度洋板块的交汇处，最初形成于古近纪，是一个大陆裂谷盆地，叠加在以剪应力为特征的背景上。复杂，使这一特征不同于典型的裂谷盆地。

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来源
《International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Cooperation among Institutions of Higher Education: Extended Abstract Volume》|2014年|37-38|共2页
会议地点 Wuhan(CN)
作者
Hailun Liu;
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作者单位

Faculty of Earth Resources, China University of Geosciences, Wuhan, Hubei, 430074, China;

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会议组织
原文格式 PDF
正文语种 eng
中图分类矿山设计与建设;
关键词
Huizhou depression; Paleogene; faulting and uplift;

机译：惠州洼地；古近纪；断层隆升;

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Analysis of the mechanism of faulting and uplift in the Huizhou depression, Pearl River Delta, South China

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