贵州花溪P-T界线附近粘土矿物结构及成因意义

高文鹏; 洪汉烈; 殷科; 赖旭龙; 王朝文; 李荣彪; 杨博; 韩文; 刘欣

doi:10.3799/dqkx.2013.122

Volume 38 Issue 6

Jun. 2013

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Article Navigation > Earth Science > 2013 > 38(6): 1253-1262

GAO Wen-peng, HONG Han-lie, YIN Ke, Lai Xu-long, WANG Chao-wen, LI Rong-biao, Yang Bo, HAN Wen, LIU Xin, 2013. Fine Structure and Their Genetic Significance of Clay Minerals from the Permian-Triassic Boundary, Huaxi Area, Guizhou Province. Earth Science, 38(6): 1253-1262. doi: 10.3799/dqkx.2013.122

Citation:

GAO Wen-peng, HONG Han-lie, YIN Ke, Lai Xu-long, WANG Chao-wen, LI Rong-biao, Yang Bo, HAN Wen, LIU Xin, 2013. Fine Structure and Their Genetic Significance of Clay Minerals from the Permian-Triassic Boundary, Huaxi Area, Guizhou Province. Earth Science, 38(6): 1253-1262. doi: 10.3799/dqkx.2013.122

Citation:

GAO Wen-peng, HONG Han-lie, YIN Ke, Lai Xu-long, WANG Chao-wen, LI Rong-biao, Yang Bo, HAN Wen, LIU Xin, 2013. Fine Structure and Their Genetic Significance of Clay Minerals from the Permian-Triassic Boundary, Huaxi Area, Guizhou Province. Earth Science, 38(6): 1253-1262. doi: 10.3799/dqkx.2013.122

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Fine Structure and Their Genetic Significance of Clay Minerals from the Permian-Triassic Boundary, Huaxi Area, Guizhou Province

doi: 10.3799/dqkx.2013.122

GAO Wen-peng^1
,,
HONG Han-lie^{1, 2
,
,},
YIN Ke¹,
Lai Xu-long^{1, 2},
WANG Chao-wen¹,
LI Rong-biao¹,
Yang Bo¹,
HAN Wen¹,
LIU Xin¹

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-12-10
Publish Date: 2013-06-01

Abstract

Abstract

The fine structure and provenance of clays across the Permian-Triassic boundary (PTB) in the Yanlou section were investigated by X-ray diffraction (XRD), scanning electron microscopy (SEM) and differential scanning calorimetry (DSC). The results suggest that the layers have two different provenances. The sample of YN06 exhibits a condensed texture with an oriented arrangement of detrital clay particles and consists mainly of illite and minor chlorite, with irregular outlines or ragged edges. The dehydroxylation temperature occurred at 590 ℃, indicating that clay minerals are composed of trans-vacant (tv) octahedral sheets derived from weathering of detrital illite. Other samples are composed mainly of I-S, illite and minor smectite, chlorite, with dehydroxylation temperature all above 600 ℃, suggesting that clay minerals consist of a mixture of tv and cv sheets and were derived from a mixture of terrigenous and volcanic sources.
- Permian-Triassic Boundary (PTB),
- clay minerals,
- volcanic rocks,
- fine structure

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References(54)

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Fine Structure and Their Genetic Significance of Clay Minerals from the Permian-Triassic Boundary, Huaxi Area, Guizhou Province

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