东天山哈尔里克地区早石炭世A型花岗岩年代学、地球化学及地质意义

刘鸿飞; 赵浩; 郭瑞禄; 王国灿; 廖群安

doi:10.3799/dqkx.2021.077

Volume 47 Issue 6

Jun. 2022

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Liu Hongfei, Zhao Hao, Guo Ruilu, Wang Guocan, Liao Qun’an, 2022. Geochronology, Geochemistry and Geological Implications of Early Carboniferous A-Type Granites in Harlik Area from East Tianshan. Earth Science, 47(6): 2245-2263. doi: 10.3799/dqkx.2021.077

Citation:

Liu Hongfei, Zhao Hao, Guo Ruilu, Wang Guocan, Liao Qun’an, 2022. Geochronology, Geochemistry and Geological Implications of Early Carboniferous A-Type Granites in Harlik Area from East Tianshan. Earth Science, 47(6): 2245-2263. doi: 10.3799/dqkx.2021.077

Citation:

Liu Hongfei, Zhao Hao, Guo Ruilu, Wang Guocan, Liao Qun’an, 2022. Geochronology, Geochemistry and Geological Implications of Early Carboniferous A-Type Granites in Harlik Area from East Tianshan. Earth Science, 47(6): 2245-2263. doi: 10.3799/dqkx.2021.077

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Geochronology, Geochemistry and Geological Implications of Early Carboniferous A-Type Granites in Harlik Area from East Tianshan

doi: 10.3799/dqkx.2021.077

Liu Hongfei^{1
,
,},
Zhao Hao^{2
,
,
,},
Guo Ruilu³,
Wang Guocan³,
Liao Qun’an³

1.
Hubei Institute of Geosciences, Wuhan 430034, China
2.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Institute for Advanced Ocean Study, College of Marine Geosciences, Ocean University of China, Qingdao 266237, China
3.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2021-05-24
Publish Date: 2022-06-25

Abstract

Abstract

Study of A-type granites is critical for understanding the crust-mantle interaction and tectonic evolution in the Tianshan orogenic belt. Here it reports a detailed petrologic, geochemical and geochronologic data for the alkali-feldspar granite and syenogranite from Harlik in East Tianshan, to constrain their petrogenesis and tectonic setting. LA–ICP–MS zircon U–Pb ages indicate that the granites were emplaced at early Early Carboniferous (350.7±2.0 Ma and 351.8±2.0 Ma). The rocks contain abundant alkali feldspar and biotite with little sodium amphibole. The granites are characterized by high silicon and alkali, low CaO and MgO contents, and enriched in Rb, Th, K (LILE), and Zr, Hf (HFSE), but depleted in Ba, Sr, and Eu. The chondrite-normalized REE patterns show slight enrichment in LREE with (La/Yb)_N from 3.23 to 5.55, and great negative Eu anomalies (δEu=0.19-0.28). These feactures indicate the geochemical characteristics of high-K meta- to per-aluminous A-type granite. They have positive ε_Nd(t) (+4.2 to +4.8) values, and the Neoproterozoic two stage Nd model ages (t_DM2=0.71-0.75 Ga), suggesting that the A-type granitic magma was probably generated from partial melting of a juvenile crustal source produced by depleted mantle-derived basaltic magmas and a few marine sediments. Combining with the previous works in this region, our study reveals that Harlik and Bogda are constrained by the same tectonic setting in Early Carboniferous, and the A-type granites from Harlik were genetically linked to the initial extensional stage of the Bogda back-arc rift.
- East Tianshan,
- Harlik,
- Early Carboniferous,
- A-type granite,
- zricon U-Pb dating,
- geochemistry

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References(108)

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Geochronology, Geochemistry and Geological Implications of Early Carboniferous A-Type Granites in Harlik Area from East Tianshan

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