地壳生长及深部物质架构研究与问题：以中亚造山带（北疆地区）为例

王涛; 黄河; 宋鹏; 吴欢欢; 张建军; 童英; 杜開明; 秦切

doi:10.3799/dqkx.2020.172

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2326-2344

Wang Tao, Huang He, Song Peng, Wu Huanhuan, Zhang Jianjun, Tong Ying, Du Kaiming, Qin Qie, 2020. Studies of Crustal Growth and Deep Lithospheric Architecture and New Issues: Exemplified by the Central Asian Orogenic Belt (Northern Xinjiang). Earth Science, 45(7): 2326-2344. doi: 10.3799/dqkx.2020.172

Citation:

Wang Tao, Huang He, Song Peng, Wu Huanhuan, Zhang Jianjun, Tong Ying, Du Kaiming, Qin Qie, 2020. Studies of Crustal Growth and Deep Lithospheric Architecture and New Issues: Exemplified by the Central Asian Orogenic Belt (Northern Xinjiang). Earth Science, 45(7): 2326-2344. doi: 10.3799/dqkx.2020.172

Citation:

Wang Tao, Huang He, Song Peng, Wu Huanhuan, Zhang Jianjun, Tong Ying, Du Kaiming, Qin Qie, 2020. Studies of Crustal Growth and Deep Lithospheric Architecture and New Issues: Exemplified by the Central Asian Orogenic Belt (Northern Xinjiang). Earth Science, 45(7): 2326-2344. doi: 10.3799/dqkx.2020.172

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Studies of Crustal Growth and Deep Lithospheric Architecture and New Issues: Exemplified by the Central Asian Orogenic Belt (Northern Xinjiang)

doi: 10.3799/dqkx.2020.172

Wang Tao^{1, 2, 3
,
,},
Huang He^{1, 3},
Song Peng^{1, 3},
Wu Huanhuan^{1, 4},
Zhang Jianjun^{1, 3},
Tong Ying^{1, 3},
Du Kaiming^{1, 4},
Qin Qie^{1, 3}

1.
Key Laboratory of the Deep Earth Geodynamics, Ministry of Natural Resources, Beijing 100037, China
2.
Beijing SHRIMP Center, Beijing 100037, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
4.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100038, China

Received Date: 2020-06-23
Publish Date: 2020-07-15

Abstract

Abstract

Multiple isotopic mapping of magmatic rocks is a useful tool to unveil the architecture and composition of the deep lithosphere of orogens and to study the crustal growth. As the world's largest and most typical accretionary orogenic belt,the Central Asian Orogenic Belt (CAOB) is an ideal natural laboratory for addressing the scientific issues mentioned above. In this contribution,we synthetically exhibit the recent achievements in isotopic mapping being carried out in northern Xinjiang,SW CAOB,and discuss the relevant issues. Cross-section of Nd-Hf isotopic data across the Altai-Junggar-Tianshan-Beishan orogens preliminarily indicate that some ancient materials are distributed in the central Altai,the Junggar is composed mostly of juvenile components,and the most ancient crustsare found in Eastern Tianshan-Beishan areas. These differences can be attributed to the combination of lateral continental crust growth at the syn-accretionary stage and the vertical growth at late- to post-accretionary stages. The Hf isotopic mapping of felsic rocks in the Western Tianshan and adjacent regions reveals a within-microcontinental heterogeneity in lithospheric architecture,and alternating occurrence in space and time of juvenile and ancient crustal components implies periodic continental growth and reworking. Details of components in the deep lithosphere probed by isotopic mapping,juvenile crustal endmembers particularly,require further studies. We need to explore the results of multi-proxy isotopicsystems and understand the mechanism behind the similarities and differences. Furthermore,deep lithospheric compositions traced by multi-isotopes should be in agreement with geophysical data as well as experimental petrology. Our ultimate goal is to establish a multidisciplinary approach with multi-isotopic mapping as the core,including geophysical detection,deep drilling,and simulation of deep process.
- magmatic rocks,
- isotope mapping,
- deep lithospheric architecture,
- Central Asia (Northern Xinjiang),
- geophysics

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References(109)

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Studies of Crustal Growth and Deep Lithospheric Architecture and New Issues: Exemplified by the Central Asian Orogenic Belt (Northern Xinjiang)

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