Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block

XU ZhengYu; JIANG Shu; XIONG ShaoYun; LIANG Xing; WANG GaoCheng; GUO YanLing; HE Yong; RAO DaQian

doi:10.14027/j.cnki.cjxb.2015.01.003

Volume 33 Issue 1

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XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003

Citation:

XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003

Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block

doi: 10.14027/j.cnki.cjxb.2015.01.003

1.
Hangzhou Research Institute of Petroleum Geology, PetroChina, Hangzhou 310023;
2.
Energy & Geoscience Institute (EGI), University of Utah, Salt Lake City, UT 84108;
3.
Zhejiang Oilfield company, PetroChina, Hangzhou 310013

Received Date: 2014-02-24
Rev Recd Date: 2014-04-25
Publish Date: 2015-02-10

Abstract

To further investigate the Paleozoic organic-rich shale development and distribution characteristics in the Yangtze Continental Block, and the depositional model, we systematically collected and compiled large data sets of organic-rich shales for the Lower Cambrian Niutitang equivalent Formation and Upper Ordovician Wufeng-Lower Silurian Longmaxi equivalent Formation. Outcrop in Zhalagou of Sandu county, Guizhou province and Zhao 104 wells Junlian Prefecture, Sichuan Province were selected for the systematic observation, sample tests, sedimentary facies, and so on. Regional reconstruction of paleogeography and correlation between different regions show that the Yangtze block was passive continental margin during the early Paleozoic and peripheral foreland during early Silurian. Niutitang equivalent shales were deposited in a passive continental margin environment, the upwelling nutrient flow and anoxic events in complex depositional model is interpreted for the depositional model of Lower Cambrian shale in Yangtze Block, organic-rich thick shale was mainly developed in the southeastern margin of the Yangtze block deep water shelf to slope facies; Ordovician Wufeng- Lower Silurian Longmaxi equivalent shales were deposited in the Caledonian orogenic front of the periphery foreland environment, organic-rich thick shale was mainly developed in in the anoxic intra-shelf low setting in southeastern margin of the Upper to middle Yangtze block.
- depositional model,
- development characteristic,
- organic rich shale,
- Early Paleozoic,
- Yangtze Continental Block

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通讯作者: 陈斌, bchen63@163.com

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沈阳化工大学材料科学与工程学院沈阳 110142

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Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block

1. Hangzhou Research Institute of Petroleum Geology, PetroChina, Hangzhou 310023;

2. Energy & Geoscience Institute (EGI), University of Utah, Salt Lake City, UT 84108;

3. Zhejiang Oilfield company, PetroChina, Hangzhou 310013

Received Date: 2014-02-24

Rev Recd Date: 2014-04-25

Publish Date: 2015-02-10

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Abstract: To further investigate the Paleozoic organic-rich shale development and distribution characteristics in the Yangtze Continental Block, and the depositional model, we systematically collected and compiled large data sets of organic-rich shales for the Lower Cambrian Niutitang equivalent Formation and Upper Ordovician Wufeng-Lower Silurian Longmaxi equivalent Formation. Outcrop in Zhalagou of Sandu county, Guizhou province and Zhao 104 wells Junlian Prefecture, Sichuan Province were selected for the systematic observation, sample tests, sedimentary facies, and so on. Regional reconstruction of paleogeography and correlation between different regions show that the Yangtze block was passive continental margin during the early Paleozoic and peripheral foreland during early Silurian. Niutitang equivalent shales were deposited in a passive continental margin environment, the upwelling nutrient flow and anoxic events in complex depositional model is interpreted for the depositional model of Lower Cambrian shale in Yangtze Block, organic-rich thick shale was mainly developed in the southeastern margin of the Yangtze block deep water shelf to slope facies; Ordovician Wufeng- Lower Silurian Longmaxi equivalent shales were deposited in the Caledonian orogenic front of the periphery foreland environment, organic-rich thick shale was mainly developed in in the anoxic intra-shelf low setting in southeastern margin of the Upper to middle Yangtze block.

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[83]	陈旭,张元动,樊隽轩,等. 广西运动的进程: 来自生物相和岩相带的证据[J]. 中国科学(D辑): 地球科学,2012,42(11): 1617-1626.[Chen Xu, Zhang Yuandong, Fan Junxuan, et al. Process of Guangxi movement: Evidence from biological phase and facies belts [J]. Science China(Series D): Earth Sciences, 2012, 42(11): 1617-1626.]
[84]	刘树根,王世玉,孙玮,等. 四川盆地及其周缘五峰组龙马溪组黑色页岩特征[J]. 成都理工大学学报: 自然科学版,2013,40(6): 621-639.[Liu Shugen, Wang Shiyu, Sun Wei, et al. Characteristics of block shale in Wufeng Formation and Longmaxi Formation in Sichuan Basin and its peripheral areas[J]. Journal of Chengdu University of Technology: Science and Technology Edition, 2013, 40(6): 621-639.]
[85]	陈旭,戎嘉余. 从生物地层学到大地构造学——以华南奥陶系和志留系为例[J]. 现代地质,1999,13(4): 385-389.[Chen Xu, Rong Jiayu. From biostratigraphy to tectonics—with Ordovician and Silurian of South China as an example[J]. Geoscience, 1999, 13(4): 385-389.]
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Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block

doi: 10.14027/j.cnki.cjxb.2015.01.003

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通讯作者: 陈斌, bchen63@163.com

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