北羌塘三叠纪辉石闪长玢岩的成因及其地球动力学背景

杨凯; 刘彬; 马昌前; 孙洋; 张飞; 牟进忠; 何雨; 肖露

doi:10.3799/dqkx.2019.163

Volume 45 Issue 5

May 2020

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Yang Kai, Liu Bin, Ma Changqian, Sun Yang, Zhang Fei, Mou Jinzhong, He Yu, Xiao Lu, 2020. Petrogenesis and Geodynamic Setting of Triassic Pyroxene Diorite-Porphyrite from the North Qiangtang Terrane: Geochronology, Mineral Petrogeochemistry and Sr-Nd-Hf Isotope Constraints. Earth Science, 45(5): 1490-1502. doi: 10.3799/dqkx.2019.163

Citation:

Yang Kai, Liu Bin, Ma Changqian, Sun Yang, Zhang Fei, Mou Jinzhong, He Yu, Xiao Lu, 2020. Petrogenesis and Geodynamic Setting of Triassic Pyroxene Diorite-Porphyrite from the North Qiangtang Terrane: Geochronology, Mineral Petrogeochemistry and Sr-Nd-Hf Isotope Constraints. Earth Science, 45(5): 1490-1502. doi: 10.3799/dqkx.2019.163

Citation:

Yang Kai, Liu Bin, Ma Changqian, Sun Yang, Zhang Fei, Mou Jinzhong, He Yu, Xiao Lu, 2020. Petrogenesis and Geodynamic Setting of Triassic Pyroxene Diorite-Porphyrite from the North Qiangtang Terrane: Geochronology, Mineral Petrogeochemistry and Sr-Nd-Hf Isotope Constraints. Earth Science, 45(5): 1490-1502. doi: 10.3799/dqkx.2019.163

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Petrogenesis and Geodynamic Setting of Triassic Pyroxene Diorite-Porphyrite from the North Qiangtang Terrane: Geochronology, Mineral Petrogeochemistry and Sr-Nd-Hf Isotope Constraints

doi: 10.3799/dqkx.2019.163

Yang Kai^{1, 2, 3
,},
Liu Bin^{1, 2, 4
,
,},
Ma Changqian⁴,
Sun Yang^{1, 4},
Zhang Fei⁵,
Mou Jinzhong¹,
He Yu¹,
Xiao Lu¹

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China
3.
School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
4.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
5.
School of Energy Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2019-07-08
Publish Date: 2020-05-15

Abstract

Abstract

Although large volume of Triassic magmatism has been identified in the central Tibetan Plateau,the petrogenesis and geodynamic setting of these igneous rocks are still poorly understood. In this paper,we carried out a detailed study of zircon U-Pb geochronology,petrology,and geochemisrty for the diorite porphyrite in North Qiangtang terrane,aiming to reveal its petrogenesis and constaint the exploration of the Triassic tectonic-magmatic evolution. The LA-ICP-MS zircon U-Pb dating for this magmatic rock yields a crystallization age of 227±2 Ma (MSWD=0.86). All the samples have high contents of silicon and aluminum and belong to calc-alkaline series in composition. Compared with the primitive mantle,they exhibit enrichment of LREE,Th,and U,with depletion of Nb,Ta and Ti. All the samples have relatively low ε_Nd(t) values (-4.53 to -4.99),relatively concentrated I_Sr values (0.707 05 to 0.707 14),and positive ε_Hf(t) values (+0.81 to +2.48),suggesting an enriched mantle. Geochemical and isotopic variations reveal that the diorite-porphyrite was derived from partial melting of an enriched mantle that was previously modified by subduction-related components(e.g.,sediments). In addition,combined with the existing multi-disciplinary research data in the region,it could be concluded that the subduction of the Paleo-Tethyan ocean in the North Qiangtang terrane lasted at least to 227 Ma.
- Triassic,
- diorite-porphyrite,
- petrogenesis,
- Paleo-Tethyan Ocean,
- North Qiangtang terrane,
- petrology

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References(73)

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