北喜马拉雅佩枯花岗岩年代学、成因机制及其构造意义

王晓先; 张进江; 王佳敏

doi:10.3799/dqkx.2016.082

Volume 41 Issue 6

Jun. 2016

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Wang Xiaoxian, Zhang Jinjiang, Wang Jiamin, 2016. Geochronology and Formation Mechanism of the Paiku Granite in the Northern Himalaya, and Its Tectonic Implications. Earth Science, 41(6): 982-998. doi: 10.3799/dqkx.2016.082

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Wang Xiaoxian, Zhang Jinjiang, Wang Jiamin, 2016. Geochronology and Formation Mechanism of the Paiku Granite in the Northern Himalaya, and Its Tectonic Implications. Earth Science, 41(6): 982-998. doi: 10.3799/dqkx.2016.082

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Geochronology and Formation Mechanism of the Paiku Granite in the Northern Himalaya, and Its Tectonic Implications

doi: 10.3799/dqkx.2016.082

Wang Xiaoxian^{1,2,3,4
,},
Zhang Jinjiang^3,4,
Wang Jiamin^3,4

1.
Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
2.
Key Laboratory of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
3.
School of Earth and Space Sciences, Peking University, Beijing 100871, China
4.
Key Laboratory of Orogenic Belts and Crustal Evolution of the Ministry of Education, Peking University, Beijing 100871, China

Received Date: 2015-12-16
Publish Date: 2016-06-15

Abstract

Abstract

Situated in the middle of Tethyan Himalaya, northern Himalayan granites not only better our understanding of melting behaviors and mechanism of the crust during the collisional orogenic processes, but also facilitate the investigation and evaluation of tectonic-magmatic evolution of the Himalayan orogen.In this paper, we present geochronological, geochemical and Sr-Nd isotopic data of the Paiku granites in the northern Himalaya.LA-MC-ICP-MS zircon U-Pb dating reveals that Paiku granites were crystallized from 23.9 Ma to 16.5 Ma and have experienced at least two episodes of anatexis at 22.3±0.6 Ma and 17.3±0.3 Ma, respectively. The age of 17.3±0.3 Ma probably represents the final crystallized timing.Bulk-rock major and trace elements analyses indicate that Paiku granites were characterized by high SiO₂(71.87% to 75.56%), Al₂O₃(13.57% to 15.49%), K₂O(3.34% to 4.59%), and high values of K₂O/Na₂O(1.02 to 1.39), A/CNK(1.21 to 1.23), and enrichment in Rb, Th, U, depletion in Ba, Nb, Sr, Zr and no or weak negative Eu anomalies ((La/Yb)_N=10.76-16.60), and strong fractionation between LREE and HREE (δEu=0.76-0.97). These features demonstrate that Paiku granites belong to high potassium Calc-alkaline and peraluminous granites. The values of (⁸⁷Sr/⁸⁶Sr)_i and ε_Nd(t) range from 0.736 184 to 0.741 258 and from -14.6 to -14.3, and can compare well with the metasedimentary rock in the Greater Himalaya Crystalline complex (GHC). It is inferred that the Paiku granites were generated from partial melting of the GHC metasedimentary rocks. The granites show relatively high Sr, but low Rb and Rb/Sr which are nearly constant relative to large variations in Ba concentrations. These features are concordant with the trend of fluxed muscovite partial melting. Based on above evidences, we suggest the Paiku granites were derived from fluxed partial melting of the GHC metasedimentary rock, possibly related closely with the structural activity along the South Tibet detachment system (STDS).
- the northern Himalaya,
- Paiku granites,
- geochronology,
- geochemistry,
- Sr-Nd isotopes,
- formation mechanism

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References(100)

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Geochronology and Formation Mechanism of the Paiku Granite in the Northern Himalaya, and Its Tectonic Implications

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