秦祁昆接合部二叠纪沉积建造时空分布

寇晓虎; 张克信; 林启祥; 朱云海; 陈奋宁; 罗根明; 徐亚东

Volume 32 Issue 5

Sep. 2007

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Article Navigation > Earth Science > 2007 > 32(5): 681-690

KOU Xiao-hu, ZHANG Ke-xin, LIN Qi-xiang, ZHU Yun-hai, CHEN Fen-ning, LUO Gen-ming, XU Ya-dong, 2007. The Distribution of Permian Sedimentary Sequences in the Adjacent Area of Qinling-Qilian-Kunlun. Earth Science, 32(5): 681-690.

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The Distribution of Permian Sedimentary Sequences in the Adjacent Area of Qinling-Qilian-Kunlun

KOU Xiao-hu^{1, 2
,},
ZHANG Ke-xin^{1, 2},
LIN Qi-xiang²,
ZHU Yun-hai^{1, 2},
CHEN Fen-ning^{1, 2},
LUO Gen-ming^{1, 2},
XU Ya-dong^{1, 2}

1.
GPMR an d BGEG Labora tories, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2007-06-16
Publish Date: 2007-09-25

Abstract

Abstract

The study area is located in the copulae of Qinling-Qilian-Kunlun and adjacent area. In Permian, with the borderline of tectonic-stratigraphic belt in South Qilian, the south is marine facies sediment environment and the north is continental facies sediment environment: In the middle Qilian, North Qilian and Alashan of north district, the sediment is conglomerate, sandstone and mudstone, and it belong to fluvial and lacustrine facies sediment environment; In the south Qilian of mid-district, the sediment environment is belong to marine continental alternation facies with clastic rocks and limestone; In the West Qinling and East Kunlun of the south district, the sediment environment is archipelagic ocean including turbidite rocks of bathyal facies and abyssal facies, basalt, seamount carbonate and so on. During the geological mapping of 1∶250 000 Linxia city and Dingxi City, we found small ocean basin and carbonate seamount formation of early and middle Permian between West Qinling in Ganjia, Xiahe County, Gansu Province. And this can contrast with the archipelagic ocean sediment formation between Qinling and Kunlun in the area of Buqingshan-Huashixia-Xinghai. In late Permian, the sediment is still turbidite rocks of half-sea and deep-sea between Qinling and Qilian, but it is foreland-molasses sediment formation between Qinling and Kunlun.
- Qinling-Qilian-Kunlun,
- Permian,
- Sedimentary formation,
- Archipelagic Ocean.

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References(52)

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The Distribution of Permian Sedimentary Sequences in the Adjacent Area of Qinling-Qilian-Kunlun

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