QUERY ON THE NEOCATHAYSIAN FROM THE CONTRAST WITH SICHUAN BASIN AND JIANGHAN SUBSIDENCE AREA

LIN Zong-man

2014 Vol. 20, No. 3

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LIN Zong-man. QUERY ON THE NEOCATHAYSIAN FROM THE CONTRAST WITH SICHUAN BASIN AND JIANGHAN SUBSIDENCE AREA[J]. Journal of Geomechanics, 2014, 20(3): 205-221.

Citation:

LIN Zong-man. QUERY ON THE NEOCATHAYSIAN FROM THE CONTRAST WITH SICHUAN BASIN AND JIANGHAN SUBSIDENCE AREA[J]. Journal of Geomechanics, 2014, 20(3): 205-221.

QUERY ON THE NEOCATHAYSIAN FROM THE CONTRAST WITH SICHUAN BASIN AND JIANGHAN SUBSIDENCE AREA

LIN Zong-man

Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received Date: 15 May 2014

Publish Date: 25 September 2014

Abstract

Abstract

The Sichuan Basin which superimposed on the upper Yangtze Paraplatform during Late Triassic-Jurassic is a large downwarping basin, being a typical basin in the third subsidence zone in Cathaysian.The Jianghan subsidence which superimposed on the fold belt of middle Yangtze during Cretaceous to Tertiary is a rift zone, and is a typical subsidence zone of the second subsidence belt of Neocathaysian. They belong to different basins in time and characteristics, and have extensive structural unconformity. The Neocathaysian three uplifts and three depressions, which put forward by Professor LI Si-guang, is a huge complex tectonic zone, and include stacked composite between Cathaysian and Neocathaysian. The research results prove that the Meso-cathaysian did not exist, for it is just a variation of Cathaysian. In order to correctly describe the basic tectonic characteristics of Eastern China, it's necessary to further clarify the meaning of Cathaysian and Neocathaysian.
- Sichuan Basin /
- Jianghan subsidence zone /
- Eastern China /
- Cathaysian /
- Neocathaysian /
- structural unconformity

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References

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