南天山早二叠世Ⅰ型花岗岩Sr-Nd-Hf同位素特征:岩石成因和大陆地壳增长的意义

陶再礼; 尹继元; 陈文; 李大鹏; 徐志华; 杜秋怡

doi:10.3799/dqkx.2019.079

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3565-3582

Tao Zaili, Yin Jiyuan, Chen Wen, Li Dapeng, Xu Zhihua, Du Qiuyi, 2019. Sr-Nd-Hf Isotopic Characteristics of Early Permian Ⅰ-Type Granites in Southern Tianshan: Petrogenesis and Implications for Continental Crustal Growth. Earth Science, 44(10): 3565-3582. doi: 10.3799/dqkx.2019.079

Citation:

Tao Zaili, Yin Jiyuan, Chen Wen, Li Dapeng, Xu Zhihua, Du Qiuyi, 2019. Sr-Nd-Hf Isotopic Characteristics of Early Permian Ⅰ-Type Granites in Southern Tianshan: Petrogenesis and Implications for Continental Crustal Growth. Earth Science, 44(10): 3565-3582. doi: 10.3799/dqkx.2019.079

Citation:

Tao Zaili, Yin Jiyuan, Chen Wen, Li Dapeng, Xu Zhihua, Du Qiuyi, 2019. Sr-Nd-Hf Isotopic Characteristics of Early Permian Ⅰ-Type Granites in Southern Tianshan: Petrogenesis and Implications for Continental Crustal Growth. Earth Science, 44(10): 3565-3582. doi: 10.3799/dqkx.2019.079

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Sr-Nd-Hf Isotopic Characteristics of Early Permian Ⅰ-Type Granites in Southern Tianshan: Petrogenesis and Implications for Continental Crustal Growth

doi: 10.3799/dqkx.2019.079

Tao Zaili^{1,2
,},
Yin Jiyuan^{1
,
,},
Chen Wen¹,
Li Dapeng²,
Xu Zhihua^1,2,
Du Qiuyi¹

1.
Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2019-04-12
Publish Date: 2019-11-11

Abstract

Abstract

The Late Carboniferous-Early Permian granitic intrusions extensively occur in the southern Tianshan block, whereas the petrogenesis of these granites and their tectonic setting remain controversial. In this paper, it reports new zircon U-Pb age, and geochemical and Sr-Nd compositions and zircon Hf isotopic compositions of the biotite monzonitic granites in the southern Tianshan block. Based on LA-ICP-MS U-Pb zircon dating, the biotite monzonitic granites were emplaced at 295.8±1.7 Ma. They are characterized by slightly peraluminous (A/CNK=1.02-1.04), rich alkali (K₂O+Na₂O=7.49%-8.78%) and potassium-rich (K₂O/Na₂O=1.05-1.53), belonging to high potassium calc-alkaline affinity, consistent with the geochemical features of Ⅰ-type granites. They are enriched in LILEs and LREEs, depleted in HFSEs (e.g., Nb, Ta, Ti), medium-negative Eu anomalies (δEu=0.38-0.57), and predominately negative Sr, Ba anomalies. In addition, most of the biotite monzonitic granites show high initial (⁸⁷Sr/⁸⁶Sr)_i ratios, negative ε_Nd(t) and ε_Hf(t) values and few samples with low and positive ε_Nd(t) and ε_Hf(t) values, suggesting that they were produced by mixing of mafic melt-derived mantle and felsic melt derived ancient (Paleo-Mesoproterozoic) crust, with minor involvement of the Neoproterozoic crustal material, and that the crystal fractionation of plagioclase could have occurred before the parental magma emplaced. In association with previous analysis, it is proposed that the Late Carboniferous-Early Permian magmatism in the southern Tianshan block might be related to mixing of melt-derived Precambrian basement and melt-derived mantle induced by the slab roll-back of the subducted southern Tianshan oceanic lithosphere and asthenosphere upwelling. The Phanerozoic magmatic source of the southern Tianshan block is mainly characterized by the reworking of ancient crust. Compared to other regions of CAOB, there is no excessive juvenile crustal growth in the southern Tianshan.
- southern Tianshan,
- Ⅰ-type granite,
- tectonic setting,
- slab roll-back,
- magma mixing,
- petrology

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References(72)

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Sr-Nd-Hf Isotopic Characteristics of Early Permian Ⅰ-Type Granites in Southern Tianshan: Petrogenesis and Implications for Continental Crustal Growth

doi: 10.3799/dqkx.2019.079

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通讯作者: 陈斌, bchen63@163.com

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