东昆仑诺木洪地区白沙河岩组岩石学、地球化学及年代学特征

周文孝; 赵晓成; 吕新彪

doi:10.3799/dqkx.2020.313

Volume 45 Issue 12

Dec. 2020

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Zhou Wenxiao, Zhao Xiaocheng, Lü Xinbiao, 2020. Petrology, Geochemistry and Chronology of the Baishahe Formation in Numohong Area of Eastern Kunlun Orogenic Belt. Earth Science, 45(12): 4370-4388. doi: 10.3799/dqkx.2020.313

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Zhou Wenxiao, Zhao Xiaocheng, Lü Xinbiao, 2020. Petrology, Geochemistry and Chronology of the Baishahe Formation in Numohong Area of Eastern Kunlun Orogenic Belt. Earth Science, 45(12): 4370-4388. doi: 10.3799/dqkx.2020.313

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Petrology, Geochemistry and Chronology of the Baishahe Formation in Numohong Area of Eastern Kunlun Orogenic Belt

doi: 10.3799/dqkx.2020.313

Zhou Wenxiao^{1
,
,},
Zhao Xiaocheng²,
Lü Xinbiao^{1, 3, 4
,
,}

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
Xinjiang Earthquake Administration, China Earthquake Administration, Urumqi 830011, China
3.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2020-07-19
Publish Date: 2020-12-15

Abstract

Abstract

The Baishahe Formation in the lower part of the Jinshuikou Group is one of the basement metamorphic rock series in the East Kunlun,which has essential geological significance for studying the formation and evolution of the East Kunlun orogenic belt. In this paper,the Baishahe Formation exposed in the Nuomuhong area of Qinghai Province was selected as the object of study,which was investigated by geological field survey,petrology,whole-rock geochemistry,zircon U-Pb chronology,etc. The Baishahe rock group in the area was divided into three lithologic sections through investigation. Characteristic metamorphic mineral combinations such as sillimanite,garnet,monoclinic pyroxene,and dolomite were identified. This indicats that the rock group had experienced high amphibolite facies-low granulite facies metamorphism. For the identified argillaceous metamorphic rocks,the apparent peak metamorphic temperature and pressure recovered by the garnet-biotite thermometer and garnet-biotite-plagioclase-quartz manometer are 660-683 ℃,and 3.9-4.2 kbar,respectively. For basic metamorphic rocks,the metamorphic temperature and temperature recovered using hornblende-plagioclase thermometer and hornblende-plagioclase-quartz manometer are 723-772 ℃ and 3.4-4.9 kbar,respectively. The paragneiss was studied using clastic zircon chronology. Results show that the frequency peak concentrated at 1 300 Ma,and the original rock sedimentation age should be later than the Mesoproterozoic. The original rocks were recovered using rock geochemical data. The original rocks of the basic metamorphic rock in the Baishahe Formation were determined to be tholeiitic basalt formed in the extensional environment within the plate; the original rocks of the felsic metamorphic rock were identified as muddy-sand continental marginal clastic rock. The original rocks of the Baishahe Formation are constructed of continental marginal clastic rocks with basic volcanic rocks,with carbonate deposits in the upper part. It may have been formed in the late stage of continental rifting and under the tectonic environments from extension to compression.
- East Kunlun,
- Jinshuikou Group,
- Baishahe Formation,
- Mesoproterozoic,
- metamorphic temperature and pressure conditions,
- zircon U-Pb,
- chronology

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References(83)

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Petrology, Geochemistry and Chronology of the Baishahe Formation in Numohong Area of Eastern Kunlun Orogenic Belt

doi: 10.3799/dqkx.2020.313

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