东昆仑古特提斯构造带中的原特提斯记录:来自苦海镁铁质岩块的证据

张航; 王宗起; 马昌前; 熊富浩; 蒋红安; 郭宇衡

doi:10.3799/dqkx.2018.714

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1164-1182

Zhang Hang, Wang Zongqi, Ma Changqian, Xiong Fuhao, Jiang Hong'an, Guo Yuheng, 2018. Proto-Tethys Record in Paleo-Tethys Belt of East Kunlun: Evidence from Kuhai Mafic Blocks. Earth Science, 43(4): 1164-1182. doi: 10.3799/dqkx.2018.714

Citation:

Zhang Hang, Wang Zongqi, Ma Changqian, Xiong Fuhao, Jiang Hong'an, Guo Yuheng, 2018. Proto-Tethys Record in Paleo-Tethys Belt of East Kunlun: Evidence from Kuhai Mafic Blocks. Earth Science, 43(4): 1164-1182. doi: 10.3799/dqkx.2018.714

Citation:

Zhang Hang, Wang Zongqi, Ma Changqian, Xiong Fuhao, Jiang Hong'an, Guo Yuheng, 2018. Proto-Tethys Record in Paleo-Tethys Belt of East Kunlun: Evidence from Kuhai Mafic Blocks. Earth Science, 43(4): 1164-1182. doi: 10.3799/dqkx.2018.714

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Proto-Tethys Record in Paleo-Tethys Belt of East Kunlun: Evidence from Kuhai Mafic Blocks

doi: 10.3799/dqkx.2018.714

1.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
4.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
5.
Changsha Uranium Geology Research Institute No. 230, CNNC, Changsha 410011, China
6.
Sichuan Institute of Land Planning and Survey, Chengdu 610000, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

The junction of the East Kunlun orogen and the West Qinling orogen is a key area for contrasting the tectonic evolution of the East Kunlun orogen with West Qinling orogen and determining the south margin of "Qinling-Qilian-Kunlun" proto-Tethys ocean. Kuhai mafic rocks, situated in the junction, were structurally placed into a Late Paleozoic foliated turbidites, indicating typical characteristics of mélange. The LA-ICP-MS zircon U-Pb dating indicates that the gabbros in Xueqiong were crystallized at 610-630 Ma, and the mafic rocks in Yari were crystallized with an age of about 504 Ma. Geochemical and isotopic studies show that Xueqiong gabbros were derived from subcontinent lithosphere mantle in a rift setting. Yari mafic rocks were derived from enrichment mantle wedge modified by subduction metasomatic fluids in subduction, representing the existence of the ocean. According to regional data analysis, the situation that proto-tethys materials mixed in paleo-tethys mélange belt may demonstrates a subduction-accretion process occurred in the junction of the East Kunlun orogen and the West Qinling orogen. From Late Neoproterozoic to the Early Palaeozoic, A'nyemaqen ocean had similar tectonic evolution with Mianlüe ocean. The margin of proto-Tethys ocean reached A'nyemaqen and Mianlüe mélange.
- Kuhai Group,
- mélange,
- zircon U-Pb chronology,
- geochemistry

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References(128)

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