帕米尔东北缘新生代隆升活动：来自奥依塔格剖面砾石统计的证据

廖林; 陈汉林; 程晓敢; 林秀斌; 赵学钦; 姚琪; 周玉彬; 白琰

doi:10.3799/dqkx.2012.088

Volume 37 Issue 4

Jul. 2012

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Article Navigation > Earth Science > 2012 > 37(4): 791-804

LIAO Lin, CHEN Han-lin, CHENG Xiao-gan, LIN Xiu-bin, ZHAO Xue-qin, YAO Qi, ZHOU Yu-bin, BAI Yan, 2012. Cenozoic Uplift of the Northeastern Pamir: Evidence from the Gravel Counting Results of the Oytag Section. Earth Science, 37(4): 791-804. doi: 10.3799/dqkx.2012.088

Citation:

LIAO Lin, CHEN Han-lin, CHENG Xiao-gan, LIN Xiu-bin, ZHAO Xue-qin, YAO Qi, ZHOU Yu-bin, BAI Yan, 2012. Cenozoic Uplift of the Northeastern Pamir: Evidence from the Gravel Counting Results of the Oytag Section. Earth Science, 37(4): 791-804. doi: 10.3799/dqkx.2012.088

Citation:

LIAO Lin, CHEN Han-lin, CHENG Xiao-gan, LIN Xiu-bin, ZHAO Xue-qin, YAO Qi, ZHOU Yu-bin, BAI Yan, 2012. Cenozoic Uplift of the Northeastern Pamir: Evidence from the Gravel Counting Results of the Oytag Section. Earth Science, 37(4): 791-804. doi: 10.3799/dqkx.2012.088

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Cenozoic Uplift of the Northeastern Pamir: Evidence from the Gravel Counting Results of the Oytag Section

doi: 10.3799/dqkx.2012.088

LIAO Lin^{1, 2
,},
CHEN Han-lin^{1, 2},
CHENG Xiao-gan^{1, 2},
LIN Xiu-bin^{1, 2},
ZHAO Xue-qin^{1, 2},
YAO Qi³,
ZHOU Yu-bin⁴,
BAI Yan⁵

1.
Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China
2.
Structural Research Center of Oil and Gas Bearing Basin of Ministry of Education, Hangzhou 310027, China
3.
Institute of Geology, China Earthquake Administration, Beijing 100029, China
4.
Southwest Oil and Gas Field Company, CNPC, Jiangyou 621709, China
5.
Yanchang Oil Field Co. Ltd., Yan'an 717600, China

Received Date: 2012-02-28
Available Online: 2021-10-13
Publish Date: 2012-07-15

Abstract

Abstract

The study of gravel-facies, an important sedimentary indicator of tectonic event could facilitate the understanding of the evolution of the uplift in orogen. In this paper, the Cenozoic gravels in Oytag section located in the piedmont of northeastern Pamir, has been chosen to conduct gravel counting. The results show that gravels in Cenozoic are mainly igneous and metamorphic, indicating that they came from Pamir area. As the first occurrence of new gravel types, the granite gravel emerges at the bottom of Atushi Formation of Pliocene. The gravels are mainly of giant-size, sub-rounded and sub-angular, moderated and middling to bad sorted, with a ratio of the length of maximum axis to the minimum axis ranging from 1 to 2. Combined with Cenozoic depositing environment and thermochronology records, following uplifting periods have been identified in northeastern Pamir as Late Oligocene to Early Miocene, Mid Miocene and since Early Pliocene.
- northeastern Pamir,
- Cenozoic,
- uplift,
- gravel counting,
- Oystag,
- sedimentology,
- tectonics

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References(92)

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Cenozoic Uplift of the Northeastern Pamir: Evidence from the Gravel Counting Results of the Oytag Section

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