东昆仑造山带东段志留纪-泥盆纪中性岩的成因及其构造意义

刘彬; 伍炼华; 马昌前; 徐雨; 李福林; 湛君明; 黄坚; 孙洋

doi:10.3799/dqkx.2022.188

Volume 48 Issue 6

Jun. 2023

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Article Navigation > Earth Science > 2023 > 48(6): 2398-2414

Liu Bin, Wu Lianhua, Ma Changqian, Xu Yu, Li Fulin, Zhan Junming, Huang Jian, Sun Yang, 2023. Petrogenesis and Tectonic Implications of Silurian to Devonian Intermediate Rocks from East Part of East Kunlun Orogenic Belt. Earth Science, 48(6): 2398-2414. doi: 10.3799/dqkx.2022.188

Citation:

Liu Bin, Wu Lianhua, Ma Changqian, Xu Yu, Li Fulin, Zhan Junming, Huang Jian, Sun Yang, 2023. Petrogenesis and Tectonic Implications of Silurian to Devonian Intermediate Rocks from East Part of East Kunlun Orogenic Belt. Earth Science, 48(6): 2398-2414. doi: 10.3799/dqkx.2022.188

Citation:

Liu Bin, Wu Lianhua, Ma Changqian, Xu Yu, Li Fulin, Zhan Junming, Huang Jian, Sun Yang, 2023. Petrogenesis and Tectonic Implications of Silurian to Devonian Intermediate Rocks from East Part of East Kunlun Orogenic Belt. Earth Science, 48(6): 2398-2414. doi: 10.3799/dqkx.2022.188

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Petrogenesis and Tectonic Implications of Silurian to Devonian Intermediate Rocks from East Part of East Kunlun Orogenic Belt

doi: 10.3799/dqkx.2022.188

Liu Bin^{1, 2
,
,},
Wu Lianhua¹,
Ma Changqian^{2, 3},
Xu Yu¹,
Li Fulin⁴,
Zhan Junming¹,
Huang Jian³,
Sun Yang¹

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
4.
Wuhan Center, China Geological Survey (Central South China Innovation Center for Geosciences), Wuhan 430205, China

Received Date: 2022-05-05
Publish Date: 2023-06-25

Abstract

Abstract

Investigations and studies on syn- exhumation or post-collisional magmatic rocks can provide key clues to understanding the crust-mantle interactions during the continental subduction and exhumation, and the tectonic evolution of collisional orogenic belts. In this paper it presents a comprehensive research of zircon U-Pb geochronology, petrology, geochemistry and isotopic geology for the syn-exhumation intermediate rocks in the east part of the East Kunlun orogenic belt. And the data could offer new insights into the generation of the syn-exhumation magmatism and the proto-Tethyan tectonic evolution. The results reveal that the Balong and Jinshuikou intermediate rocks yield zircon U-Pb ages of 420 Ma and 405 Ma, respectively, which overlap the exhumation timing of eclogites. The Balong diorite-porphyrite samples have relatively low MgO and Mg^# with high K₂O, while the Jinshuikou diorite samples have relatively high MgO and Mg^# with high Na₂O. The Balong diorite-porphyrite samples exhibit decreasing ratios of Nb/La with decreasing Mg^#, similar to the features of assimilation and fractional crystallization (AFC). And all of them are plotted on the curve of fractional crystallization. However, the Jinshuikou diorite samples do not show positive correlation between Nb/La and Mg^#, and those samples are plotted on the curve of partial melting. In addition, the Balong diorite-porphyrite samples have relatively higher I_sr ratios and lower ε_Nd(t) values than those of the Jinshuikou diorite samples. Based on the new petrological, geochemical and isotopic compositions, it concludes that the Balong diorite-porphyrite and the Jinshuikou diorite were respectively derived from basaltic magma differentiation and contamination, and partial melting of the lower crustal basaltic rocks. Combining with new regional studies, it proposes that those intermediate rocks might be formed in a post-collisional extension environment, and slab break-off is the critical factor for triggering the Silurian to Devonian syn-exhumation magmatism. The continental collision and the continental subduction in the East Kunlun region should have initiated at ~440 Ma.
- intermediate rock,
- continental exhumation,
- Silurian to Devonian,
- proto-tethys,
- East Kunlun orogenic belt,
- petrology

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References(92)

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Petrogenesis and Tectonic Implications of Silurian to Devonian Intermediate Rocks from East Part of East Kunlun Orogenic Belt

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