GEOLOGICAL EVOLUTION, NEOTECTONICS AND GENETIC MECHANISM OF THE POYANG LAKE BASIN

YANG Xiao-dong; WU Zhong-hai; ZHANG Hai-jun

Volume 22 Issue 3

Sep. 2016

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Article Navigation > Journal of Geomechanics > 2016 > 22(3): 667-684

YANG Xiao-dong, WU Zhong-hai, ZHANG Hai-jun, 2016. GEOLOGICAL EVOLUTION, NEOTECTONICS AND GENETIC MECHANISM OF THE POYANG LAKE BASIN. Journal of Geomechanics, 22 (3): 667-684.

Citation:

YANG Xiao-dong, WU Zhong-hai, ZHANG Hai-jun, 2016. GEOLOGICAL EVOLUTION, NEOTECTONICS AND GENETIC MECHANISM OF THE POYANG LAKE BASIN. Journal of Geomechanics, 22 (3): 667-684.

Citation:

YANG Xiao-dong, WU Zhong-hai, ZHANG Hai-jun, 2016. GEOLOGICAL EVOLUTION, NEOTECTONICS AND GENETIC MECHANISM OF THE POYANG LAKE BASIN. Journal of Geomechanics, 22 (3): 667-684.

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GEOLOGICAL EVOLUTION, NEOTECTONICS AND GENETIC MECHANISM OF THE POYANG LAKE BASIN

YANG Xiao-dong^{1, 2
,},
WU Zhong-hai^{2, 3
,
,},
ZHANG Hai-jun¹

1.
College of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
Key Lab of Neotectonic Movement and Geohazards, Ministry of Land and Mineral Resources, Beijing 100081, China

More Information

Received: 2016-03-07
Published: 2016-09-01

Abstract

Abstract

Combining with drilling and profile data, this paper synthesizes the sedimentary characteristics and tectonic activity characteristics of the Poyang Lake Basin and discusses the development and evolution of the basin in the tectonic background of East Asia, and also summarizes the main control faults structures and their characteristics in the basin as well as it's paleogeographic evolution in the Mesozoic and Cenozoic. Finally summarizes the main fracture of Quaternary activity and its relationship with seismic activity, and the genetic mechanism of the basin is discussed according to the existing data. Comprehensive study showed that, in the Mesozoic, the movement of Yanshan brought about a set of roughly parallel NE-SW trending fault zones in southeast of China, and resulted in the Poyang lake depression and the embryonic form of Poyang lake sedimentary basin. Then, with the change of the Ganjiang fault mode, Poyang lake basin has experienced a complex evolution process. Until the Quaternary, overall depression occurred in the middle of the basin and it continued to be deposited. After the mid Holocene, it evolved into the modern Poyang Lake.
- the Poyang Lake Basin,
- geological evolution,
- neotectonics,
- active fault,
- earthquake

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References(78)

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