扬子地块新元古代裂谷盆地莲沱组沉积分异及其物源分析

杜秋定; 王剑; 汪正江; 邓奇; 杨菲

doi:10.3799/dqkx.2020.280

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2529-2543

Du Qiuding, Wang Jian, Wang Zhengjiang, Deng Qi, Yang Fei, 2021. Depositional Differentiation and Porvenance Analysis of Liantuo Formation in Neoproterozoic Rift Basin, Yangtze Block. Earth Science, 46(7): 2529-2543. doi: 10.3799/dqkx.2020.280

Citation:

Du Qiuding, Wang Jian, Wang Zhengjiang, Deng Qi, Yang Fei, 2021. Depositional Differentiation and Porvenance Analysis of Liantuo Formation in Neoproterozoic Rift Basin, Yangtze Block. Earth Science, 46(7): 2529-2543. doi: 10.3799/dqkx.2020.280

Citation:

Du Qiuding, Wang Jian, Wang Zhengjiang, Deng Qi, Yang Fei, 2021. Depositional Differentiation and Porvenance Analysis of Liantuo Formation in Neoproterozoic Rift Basin, Yangtze Block. Earth Science, 46(7): 2529-2543. doi: 10.3799/dqkx.2020.280

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Depositional Differentiation and Porvenance Analysis of Liantuo Formation in Neoproterozoic Rift Basin, Yangtze Block

doi: 10.3799/dqkx.2020.280

Du Qiuding^{1, 2, 3, 4
,
,},
Wang Jian^{1, 2},
Wang Zhengjiang³,
Deng Qi³,
Yang Fei³

1.
School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China
2.
Qiangtang Institute of Sedimentary Basin, Southwest Petroleum University, Chengdu 610500, China
3.
Chengdu Center, China Geological Survey, Chengdu 610081, China
4.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2020-09-29
Publish Date: 2021-07-15

Abstract

Abstract

The division and correlation of the Liantuo Formation and its equivalent stratigraphic units in the Mid-Yangtze block has been one of the key problems in study of the Nanhuan System (Cryogenian) in China. In the early stage of the Neoproterozoic rift basin, tectonic-sedimentary differentiation, which made the stratigraphic sequence of the basin margin incomplete. Due to the excessive reliance on the lithostratigraphic unit comparison, which are typically related to the stratigraphic correlation between the Liantuo Formation and the Banxi Group. The geochronology and paleoenvironment of the Liantuo Formation are still highly controversial. An integrated approach of facies analysis, paleogeography, and geochronology provides new insights into the sedimentology and paleogeography in the Precambrian. The Liantuo Formation was deposited ca. 790-720 Ma, which was equivalent to the Wuqiangxi Formation in the middle-upper part of the Banxi Group. Due to the uplift and subsidence of the earth's crust, the sea water gradually overflows from south to north. Different sedimentary units of the Liantuo Formation, continental, transitional and Marine facies, have been developed from north to south in the Mid-Yangtze block. Detrital zircons from the Liantuo and Xiuning formations record that the basin experienced continuous heat uplift and stratigraphic denudation in 780-760Ma during the deposition of the Liantuo Formation, which reveals the important information about the convergence and rift events of the Yangtze and Cathaysia blocks in south China.
- geochronology and paleoenvironment,
- Liantuo Formation,
- tectono-deposition differentiation,
- porvenance,
- sedimentology

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Depositional Differentiation and Porvenance Analysis of Liantuo Formation in Neoproterozoic Rift Basin, Yangtze Block

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