塘沽地区沙河街组下部含云质泥岩主微量元素地球化学特征及地质意义

李乐; 姚光庆; 刘永河; 侯秀川; 王刚; 赵耀; 高玉洁

doi:10.3799/dqkx.2015.133

Volume 40 Issue 9

Sep. 2015

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Li Le, Yao Guangqing, Liu Yonghe, Hou Xiuchuan, Wang Gang, Zhao Yao, Gao Yujie, 2015. Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower Part of Shahejie Formation in Tanggu Area, Eastern China. Earth Science, 40(9): 1480-1496. doi: 10.3799/dqkx.2015.133

Citation:

Li Le, Yao Guangqing, Liu Yonghe, Hou Xiuchuan, Wang Gang, Zhao Yao, Gao Yujie, 2015. Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower Part of Shahejie Formation in Tanggu Area, Eastern China. Earth Science, 40(9): 1480-1496. doi: 10.3799/dqkx.2015.133

Citation:

Li Le, Yao Guangqing, Liu Yonghe, Hou Xiuchuan, Wang Gang, Zhao Yao, Gao Yujie, 2015. Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower Part of Shahejie Formation in Tanggu Area, Eastern China. Earth Science, 40(9): 1480-1496. doi: 10.3799/dqkx.2015.133

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Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower Part of Shahejie Formation in Tanggu Area, Eastern China

doi: 10.3799/dqkx.2015.133

1.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Institute of Geology, 4th Oil Production Plant, Dagang Oilfield Company, Petro China, Tianjin 300280, China
3.
Oil and Gas Evaluation Division, Dagang Oilfield Company, Petro China, Tianjin 300280, China

Received Date: 2015-04-15
Publish Date: 2015-09-15

Abstract

Abstract

Fine mudstone can record and reflect geological aspects of source and sedimentary area. A set of lacustrine dolomite-bearing mudstones is developed in Lower Shahejie Formation of Tanggu area. To understand its tectonic setting, depositional setting, weathering and provenance, the geochemical characteristics of 25 rock samples were analyzed thoroughly. With dolomite-free modification, different indices and diagrams reveal identical geological information. Active continental margin setting (Andean-type) is revealed by the combination of high ∑REE(154.0×10^-6-219.3×10^-6), moderate negative Eu anomaly (0.64-0.73) and tectonic setting discriminant diagram (K₂O/Na₂O-SiO₂, SiO₂/Al₂O₃-K₂O/Na₂O, and discriminant function bivariate diagram). SiO₂-(K₂O+Na₂O+Al₂O₃) bivariate discriminant diagram, equivalent B(200.17-313.21) and approximate degree of pyritization (DOP_apx) (0.02~0.38), authigenic U(0.14-1.22), U/Th(0.17-0.44) indicate arid, saline and oxic depositional condition respectively. Chemical index of alteration (CIA)(51.26-65.74), plagioclase index of alteration (PIA)(51.65-78.06), modified index of composition variation (ICV_m)(0.67-1.24) and A-CN-K diagram reflect mild to moderate weathering of source rock. Discriminant function diagram, K-Rb bivariate diagram, A-CN-K diagram, Al₂O₃/TiO₂ index(23.37-28.58), REE pattern similar to upper continental crust (UCC) and negative Eu anomaly deduce the felsic rocks as the major source for the dolomite-bearing mudstones. Under such geological constrain, it is concluded that the source materials are mostly derived from Yanshan fold and thrust belt.
- Tanggu area,
- Shahejie Formation,
- dolomite-bearing mudstone,
- geochemistry,
- depositional setting,
- sedimentology

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Major and Trace Elements Geochemistry and Geological Implications of Dolomite-Bearing Mudstones in Lower Part of Shahejie Formation in Tanggu Area, Eastern China

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