循化盆地中新世沉积物粘土矿物的特征及其古气候指示

王粉丽; 洪汉烈; 殷科; 徐耀明; 张克信; 张楗钰

doi:10.3799/dqkx.2010.096

Volume 35 Issue 5

Sep. 2010

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WANG Fen-li, HONG Han-lie, YIN Ke, XU Yao-ming, ZHANG Ke-xin, ZHANG Jian-yu, 2010. Clay Mineralogy and Its Paleoclimatic Indicator of the Miocene Sediments of Xunhua Basin. Earth Science, 35(5): 828-838. doi: 10.3799/dqkx.2010.096

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WANG Fen-li, HONG Han-lie, YIN Ke, XU Yao-ming, ZHANG Ke-xin, ZHANG Jian-yu, 2010. Clay Mineralogy and Its Paleoclimatic Indicator of the Miocene Sediments of Xunhua Basin. Earth Science, 35(5): 828-838. doi: 10.3799/dqkx.2010.096

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Clay Mineralogy and Its Paleoclimatic Indicator of the Miocene Sediments of Xunhua Basin

doi: 10.3799/dqkx.2010.096

WANG Fen-li^1
,,
HONG Han-lie^{1, 2},
YIN Ke¹,
XU Yao-ming¹,
ZHANG Ke-xin^{1, 2, 3},
ZHANG Jian-yu^{1, 2}

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Biogeology and Enviromental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Geological Survey of China University of Geosciences, Wuhan 430074, China

Received Date: 2010-05-31
Publish Date: 2010-09-01

Abstract

Abstract

To reconstruct the paleoclimate in the Miocene, clay mineralogy of the Xunhua sediments was investigated using X-ray diffraction (XRD) and scanning electron microscopy (SEM) methods. Our results show that clay minerals of the Miocene sediments are mainly illite and smectite, with minor chlorite, kaolinite, and palygorskite. The apparent changes in their relative contents and illite crystallinity suggest that warm and humid paleoclimate conditions prevailed over the period of 23.1—21.2 Ma, then the mainly cold and dry climate succeeded in the period of 21.2—14.3 Ma, with short intervals of warm and humid climate conditions. The mainly warm and humid climate dominated in the period of 14.3-10.6 Ma, and it changed into a mainly cold and dry climate in the period of 10.6—9.3 Ma. The paleoclimate of the episode of 9.3—5.2 Ma was warm and humid, and it fluctuated frequently between cold/dry and warm/humid. The rapid changes in clay indices in the curves at 21.2 Ma and 5.8 Ma probably suggest the uplift in Xunhua of Qinghai-Tibet plateau.
- clay mineral,
- crystallinity,
- Miocene,
- Xunhua basin,
- uplift

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Clay Mineralogy and Its Paleoclimatic Indicator of the Miocene Sediments of Xunhua Basin

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