北羌塘宁多地区三叠纪过铝质花岗岩的成因及其地球动力学背景

刘彬; 徐雨; 马昌前; 李福林; 赵少卿; 湛君明; 孙洋; 黄坚

doi:10.3799/dqkx.2022.191

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3296-3311

Liu Bin, Xu Yu, Ma Changqian, Li Fulin, Zhao Shaoqing, Zhan Junming, Sun Yang, Huang Jian, 2023. Petrogenesis and Geodynamic Setting of the Ningduo Peraluminous Granites from the North Qiangtang Terrane. Earth Science, 48(9): 3296-3311. doi: 10.3799/dqkx.2022.191

Citation:

Liu Bin, Xu Yu, Ma Changqian, Li Fulin, Zhao Shaoqing, Zhan Junming, Sun Yang, Huang Jian, 2023. Petrogenesis and Geodynamic Setting of the Ningduo Peraluminous Granites from the North Qiangtang Terrane. Earth Science, 48(9): 3296-3311. doi: 10.3799/dqkx.2022.191

Citation:

Liu Bin, Xu Yu, Ma Changqian, Li Fulin, Zhao Shaoqing, Zhan Junming, Sun Yang, Huang Jian, 2023. Petrogenesis and Geodynamic Setting of the Ningduo Peraluminous Granites from the North Qiangtang Terrane. Earth Science, 48(9): 3296-3311. doi: 10.3799/dqkx.2022.191

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Petrogenesis and Geodynamic Setting of the Ningduo Peraluminous Granites from the North Qiangtang Terrane

doi: 10.3799/dqkx.2022.191

Liu Bin^{1, 2
,
,},
Xu Yu¹,
Ma Changqian^{2, 3
,
,},
Li Fulin⁴,
Zhao Shaoqing¹,
Zhan Junming¹,
Sun Yang¹,
Huang Jian³

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430078, 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: 2022-03-22
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

Triassic intermediate to acid magmatism is widely distributed in the central Tibetan Plateau (including the North Qiangtang terrane). However, the magma origin, petrogenesis and geodynamic mechanism of the magmas are still poorly understood. This paper presents an integrated study of zircon U-Pb geochronology, whole-rock and isotopic geochemistry for the Ningduo peraluminous granites from the North Qiangtang terrane, aiming to provide new insights into the generation of peraluminous granites and the Triassic tectonic-magmatic evolution of the central Tibetan Plateau. The lithology of the Ningduo peraluminous granites is biotite granodiorite, which is mainly composed of plagioclase (35%-40%), quartz (25%-30%), K-feldspar (15%-20%), and biotite (5%-10%). The crystallization age of the Ningduo granites is 248±1 Ma, which could be considered as the products of the Early Triassic magmatism. The Ningduo granites have moderate contents of SiO₂ and MgO, and relatively high contents of K and Al, which can be comparable to those of typical strongly peraluminous granites. All the samples are featured with enrichment of large ion lithophile elements (e.g., Rb, K) and light rare earth elements, and depletion of high field strength elements (e.g., Nb, Ta, Ti, and P), relative to the primitive mantle. They have relatively high I_Sr ratios of 0.720-0.722, low ε_Nd(t) values of -12.4 to -12.3, and old T_2DM ages of 2.02-2.03 Ga, similar to those of the Proterozoic gneisses and Precambrian basement-derived S-type granites. The Ningduo granites have remarkable high zirconium saturation temperatures (806-845 ℃) and Ti-in-zircon temperatures (830-1 033 ℃), similar to those of typical high-temperature granites worldwide. The results indicate that the Ningduo granites were derived from partial melting of Precambrian basement rocks (greywacke and minor pelite rocks) under a high temperature condition. During the subduction of the Longmuco-Shuanghu Ocean, slab rollback triggered the back-arc extension and intense basaltic underplating, and then induced the high-temperature melting of Precambrian basement rocks.
- peraluminous granites,
- high-temperature granite,
- petrogenesis,
- Triassic,
- North Qiangtang,
- petrology,
- geochemistry

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References(82)

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Petrogenesis and Geodynamic Setting of the Ningduo Peraluminous Granites from the North Qiangtang Terrane

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