银川盆地清水营组咸化湖盆沉积特征与湖盆演化

徐清海; 吴楠; 王健; 海连富; 曹日洲

doi:10.3799/dqkx.2021.257

Volume 48 Issue 1

Jan. 2023

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Article Navigation > Earth Science > 2023 > 48(1): 317-328

Xu Qinghai, Wu Nan, Wang Jian, Hai Lianfu, Cao Rizhou, 2023. Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin. Earth Science, 48(1): 317-328. doi: 10.3799/dqkx.2021.257

Citation:

Xu Qinghai, Wu Nan, Wang Jian, Hai Lianfu, Cao Rizhou, 2023. Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin. Earth Science, 48(1): 317-328. doi: 10.3799/dqkx.2021.257

Citation:

Xu Qinghai, Wu Nan, Wang Jian, Hai Lianfu, Cao Rizhou, 2023. Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin. Earth Science, 48(1): 317-328. doi: 10.3799/dqkx.2021.257

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Sedimentary Characteristics and Lake Basin Evolution of Salinized Lake Basin of Qingshuiying Formation in Yinchuan Basin

doi: 10.3799/dqkx.2021.257

Xu Qinghai^{1
,
,},
Wu Nan^{1
,
,},
Wang Jian¹,
Hai Lianfu²,
Cao Rizhou¹

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
Mineral and Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan 750021, China

Received Date: 2021-09-14
Available Online: 2023-02-01
Publish Date: 2023-01-25

Abstract

Abstract

Thick Cenozoic strata are developed in the Yinchuan Basin, among which the Qingshuiying Formation is the period of salinized lake basin development and the most developed layer of hydrocarbon source rocks. Therefore, it is of great geological significance and exploration significance to clarify the sedimentary characteristics and lake basin evolution of the Qingshuiying Formation. In this paper, the lithology and petrographic types of the Late Paleoproterozoic Qingshuiying Formation in the Yinchuan Basin are analyzed and summarized using field outcrops, drill cores, logs and organic geochemical data to clarify the depositional environment. The sedimentary cyclogenesis of the Qingshuiying Formation was identified and classified using rock-electric characteristics and wavelet transform, and the evolution of the lake basin was analyzed on this basis. The lithology of the Qingshuiying Formation is mainly gray mudstone, brown-red mudstone, gypsum-bearing mudstone, gypsum and thin-bedded fine sandstone and siltstone, etc., and there are four types of petrographic assemblages. The Qingshuiying Formation can be divided into three four-order sedimentary cycles, corresponding to the three evolutionary stages of the salinized lake basin of the Qingshuiying Formation. SQ₁ is the development stage of the salinized lake basin at the early stage of rifting. SQ₂ is the period of strong rifting, in which the depth of the water body of the lake basin has increased, and the salinized lake is at its peak stage. SQ₃ is the period when the water body becomes shallow, in which the scope of the lake basin becomes larger, the closure weakens, and the saline lake evolves into a freshwater lake.
- Yinchuan Basin,
- Qingshuiying Formation,
- petrographic assemblage,
- sequence classification,
- salinized lake basin,
- lake basin evolution,
- paleogeography

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References(50)

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