Quaternary tectono-sedimentary evolution of Chishan Uplift in the Dongting Lake

YAO Jihua; LIU Xiaoqun; SONG Wenjie; ZHAO Wengang; LV Huizhu; SONG Wen

doi:10.16562/j.cnki.0256-1492.2019071801

Marine Geology & Quaternary Geology > 2020 > 40(5): 160-168. > DOI: 10.16562/j.cnki.0256-1492.2019071801

YAO Jihua, LIU Xiaoqun, SONG Wenjie, ZHAO Wengang, LV Huizhu, SONG Wen. Quaternary tectono-sedimentary evolution of Chishan Uplift in the Dongting Lake[J]. Marine Geology & Quaternary Geology, 2020, 40(5): 160-168. DOI: 10.16562/j.cnki.0256-1492.2019071801

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Quaternary tectono-sedimentary evolution of Chishan Uplift in the Dongting Lake

Hunan Water Resources and Hydropower Research Institute, Changsha 410007,China

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Received Date: July 17, 2019
Revised Date: September 15, 2019
Available Online: October 20, 2020

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Abstract

Abstract

Tectonic activities were reactivated since Pleistocene at the Chishan Uplift of the Dongting Lake where complicated geological phenomena are observed. As an important geological unit in the Dongting Lake, the study of the uplift and the evolutionary characteristics of the Quaternary structures and depositional systems is of great significance to the exploration of the Quaternary history of the lake. Thus, a thorough study from the perspectives of geological structure, stratigraphic framework, lithology and paleoclimate as well as cultural relics, is made by the authors in this paper. Results show that: In the late Early Pleistocene, the structural activity of Chishan uplift was first depressed and then stable, and in the early to middle Pleistocene, it was stable - depressed-stable-raised-stable. In the beginning of late Middle Pleistocene, the area with the elevation of 0 m and above of the bedrock surface of Chishan uplift had been uplifted and formed land, and human activities began to appear. At the same time, paleolithic sites were left on the top of the Quaternary strata at that time. From late Middle Pleistocene to early Holocene, the Chishan Uplift was denuded, and the aeolian deposits were deposited in the lower area of Chishan uplift.
- paleo-climate,
- cultural relics,
- aeolian deposits,
- Quaternary,
- Pleistocene,
- Chishan Uplift

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References

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