桂北中奥陶统升坪组黑色页岩沉积环境与有机质富集

余烨; 蔡灵慧; 王莉; 吴海东

doi:10.3799/dqkx.2022.485

Volume 49 Issue 7

Jul. 2024

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Yu Ye, Cai Linghui, Wang Li, Wu Haidong, 2024. Sedimentary Environment and Organic Matter Accumulation of Black Shale in Middle Ordovician Shengping Formation, Northern Guangxi. Earth Science, 49(7): 2315-2329. doi: 10.3799/dqkx.2022.485

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Yu Ye, Cai Linghui, Wang Li, Wu Haidong, 2024. Sedimentary Environment and Organic Matter Accumulation of Black Shale in Middle Ordovician Shengping Formation, Northern Guangxi. Earth Science, 49(7): 2315-2329. doi: 10.3799/dqkx.2022.485

Citation:

Yu Ye, Cai Linghui, Wang Li, Wu Haidong, 2024. Sedimentary Environment and Organic Matter Accumulation of Black Shale in Middle Ordovician Shengping Formation, Northern Guangxi. Earth Science, 49(7): 2315-2329. doi: 10.3799/dqkx.2022.485

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Sedimentary Environment and Organic Matter Accumulation of Black Shale in Middle Ordovician Shengping Formation, Northern Guangxi

doi: 10.3799/dqkx.2022.485

Yu Ye^{1, 2
,
,},
Cai Linghui^{1, 2},
Wang Li^{1
,
,
,},
Wu Haidong^{1, 2}

1.
School of Earth Sciences and Spatial Information Engineering, Hunan University of Science and Technology, Xiangtan 411201, China
2.
Hunan Provincial Key Laboratory of Shale Gas Resource Utilization, Hunan University of Science and Technology, Xiangtan 411201, China

Received Date: 2022-07-08
Available Online: 2024-08-03
Publish Date: 2024-07-25

Abstract

Abstract

In order to discuss the relationship between sedimentary enviroment and organic matter accumulation in black shale of Middle Ordovician Shengping Formation, the Xishuiyuan Section in Wenqiao Town, Quanzhou County, northern Guangxi was chosen. The organic carbon content, kerogen carbon isotope, major and trace elements were analyzed to investigate paleo-redox, paleo-productivity, hydrothermal sedimentation, clastic influx and water limitation of the Middle Ordovician sedimentary environment in the northern Guangxi. The results show that the lower member of Shengping Formation is mainly composed of mud-rich siliceous shale with TOC of 1.45%-3.04%, and the upper member is mainly composed of siliceous shale with TOC of 0.63%-2.69%. The source of organic matter in the lower member of Shengping Formation is mainly type I kerogen, while the source of organic matter in the upper member may be type II kerogen in addition to type I kerogen. The sedimentary period of Shengping Formation in northern Guangxi is a suboxic and anoxic deep-water shelf and basin facies environment. The organic matter accumulation of mud-rich siliceous shale is a dual control pattern of productivity and preservation conditions. The organic matter accumulation of siliceous shale is a preservation condition pattern.
- black shale,
- sedimentary environment,
- organic matter accumulation,
- Shengping Formation,
- northern Guangxi,
- petroleum geology

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Sedimentary Environment and Organic Matter Accumulation of Black Shale in Middle Ordovician Shengping Formation, Northern Guangxi

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