吐哈盆地台北凹陷粘土矿物纵向异常演化与成因分析

刘宝珺; 李伟; 付建奎; 岑晓春

Volume 27 Issue 5

Sep. 2002

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LIU Bao-jun, LI Wei, FU Jian-kui, CEN Xiao-chun, 2002. Genesis of Abnormal Evolution of Clay Minerals at Different Diagenetic Stages in Taibei Depression of Tuha Basin. Earth Science, 27(5): 504-508.

Citation:

LIU Bao-jun, LI Wei, FU Jian-kui, CEN Xiao-chun, 2002. Genesis of Abnormal Evolution of Clay Minerals at Different Diagenetic Stages in Taibei Depression of Tuha Basin. Earth Science, 27(5): 504-508.

LIU Bao-jun, LI Wei, FU Jian-kui, CEN Xiao-chun, 2002. Genesis of Abnormal Evolution of Clay Minerals at Different Diagenetic Stages in Taibei Depression of Tuha Basin. Earth Science, 27(5): 504-508.

Citation:

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Genesis of Abnormal Evolution of Clay Minerals at Different Diagenetic Stages in Taibei Depression of Tuha Basin

1.
Chengdu University of Technology, Chengdu 610059, China
2.
Chinese Institute of Petroleum Exploration and Development, Beijing 100083, China

Received Date: 2002-04-22
Publish Date: 2002-09-25

Abstract

Abstract

In Taibei depression, the diagenetic evolution of the clay minerals indicates that the smectite in smectite/illite mixed layer is associated with the basic normal genetic variation with depth. However, the other clay minerals are associated with various anomalous phenomena at different diagenetic stages. The detailed investigation of diagenesis in Shanshan structure indicates that several factors, such as sedimentary provenance, aqueous medium, acidic fluid generated by diagenesis of coal measure strata, organic acid generated in the course of thermal evolution and organic acid existing in oil layer, are responsible for the anomalous variation of the clay minerals at different diagenetic stages. These factors have resulted, to different extents, in anomalous development of the clay minerals at different diagenetic stages in this region.
- Taibei depression,
- clay mineral,
- anomalous evolution,
- genesis,
- provenance,
- coal measure strata,
- aqueous medium

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References(9)

References

[1]	刘宝. 沉积岩石学[M]. 北京: 地质出版社, 1980. LIU B J. Sedimentary rock[M]. Beijing: Geological Publishing House, 1980.
[2]	应凤祥. 碎屑岩成岩阶段划分规范[M]. 北京: 石油工业出版社, 1993. YING F X. Classification standard of diagenetic stages of detrital rock[M]. Beijing: Petroleum Industry Press, 1993.
[3]	应凤祥. 中国陆相碎屑岩中的自生矿物(中国油气储层研究论文集)[M]. 北京: 石油工业出版社, 1993. YING F X. Authigenic mineral of detrital rock in the continental sedimentary Basin of China[M]. Beijing: Petroleum Industry Press, 1993.
[4]	胡惟元. 贵州六枝朗岱地区上二叠统玄武岩屑砂岩成岩特征与自生矿物的成因[J]. 沉积学报, 1988, 6(3): 70-77. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198803007.htm HU W Y. Features of diagenesis and genesis of athingenic minerals in basaltic sandstones(Upper Permian Series) in the Langdai district, Liuzhi County, Guizhou[J]. Acta Sedimentologica Sinica, 1988, 6 (3): 70-77. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198803007.htm
[5]	裘怿楠, 薛叔浩, 应凤祥. 中国陆相油气储集层[M]. 北京: 石油工业出版社, 1997. QIU Y N, XUE S H, YING F X. Reservoir of oil and gas in the continental sedimentary basin of China[M]. Beijing: Petroleum Industry Press, 1997.
[6]	戴世昭. 江汉盐湖盆地石油地质[M]. 北京: 石油工业出版社, 1997. DAI S Z. Petroleum geology of Jianghan salt-lake basin[M]. Beijing: Petroleum Industry Press, 1997.
[7]	MacGowan D, Surdam R C. Difuetional carboxylic acid anions in oilfield water[J]. Organic Geochemistry, 1988, 12: 245-259. doi: 10.1016/0146-6380(88)90262-8
[8]	李伟. 塔里木盆地油田水有机地球化学特征分类及其石油地质意义[J]. 石油勘探与开发, 1996, 22: 30-35. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK506.005.htm LI W. Characteristics of organic geochemistry and classification of oil field water in Tarim basin and its petroleum geological significance[J]. Petroleum Exploration and Development, 1996, 22: 30-35. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK506.005.htm
[9]	李伟. 影响吐哈盆地储层物性的主要因素[J]. 石油勘探与开发, 1992, 19 (增刊): 230-236. LI W. Main factors affecting on the petrophysical properties of reservoir rocks in TurpanAmi basin[J]. Petroleum Exploration and Development, 1992, 19 (Suppl): 230-236.