东昆仑哈拉森地区花岗岩类岩石成因及地质意义

何成; 王力圆; 田立明; 徐净

doi:10.3799/dqkx.2018.716

Volume 43 Issue 4

Apr. 2018

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He Cheng, Wang Liyuan, Tian Liming, Xu Jing, 2018. Petrogenesis and Geological Implications of Granitoids from Halasen, East Kunlun. Earth Science, 43(4): 1207-1218. doi: 10.3799/dqkx.2018.716

Citation:

He Cheng, Wang Liyuan, Tian Liming, Xu Jing, 2018. Petrogenesis and Geological Implications of Granitoids from Halasen, East Kunlun. Earth Science, 43(4): 1207-1218. doi: 10.3799/dqkx.2018.716

He Cheng, Wang Liyuan, Tian Liming, Xu Jing, 2018. Petrogenesis and Geological Implications of Granitoids from Halasen, East Kunlun. Earth Science, 43(4): 1207-1218. doi: 10.3799/dqkx.2018.716

Citation:

He Cheng, Wang Liyuan, Tian Liming, Xu Jing, 2018. Petrogenesis and Geological Implications of Granitoids from Halasen, East Kunlun. Earth Science, 43(4): 1207-1218. doi: 10.3799/dqkx.2018.716

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Petrogenesis and Geological Implications of Granitoids from Halasen, East Kunlun

doi: 10.3799/dqkx.2018.716

He Cheng^{1,2
,},
Wang Liyuan^{3
,
,},
Tian Liming⁴,
Xu Jing⁵

1.
Hubei Key Laboratory of Earthquake Early Warning, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China
2.
Wuhan Institute of Earthquake Engineering Co., Ltd., Wuhan 430071, China
3.
College of Zijin Mining, Fuzhou University, Fuzhou 350116, China
4.
Geophysical and Geochemical Exploration Brigade of Jiangxi, Nanchang 330201, China
5.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

Received Date: 2017-12-18
Publish Date: 2018-04-15

Abstract

Abstract

A large amount of granites widely distributes in Halasen area in the East Kunlun Mountains. The study of the granites not only help us to understand the tectono-magmatic evolution history of East Kunlun orogenic belt in the Late Paleozoic and Early Mesozoic, but also provides constraints for the subduction and closed time limit of the Paleo-Tethys Ocean. In this paper, we constrain geochronology and petrogenesis of the Halasen granites by zircon U-Pb dating and geochemical analyses. The LA-ICP-MS U-Pb analyses show that the formation ages of K-feldspar granite and fine-grained monzogranite are 239.2±1.7 Ma (MSWD=0.19) and 232.4±1.2 Ma (MSWD=0.76), respectively, which are the products of the Middle Triassic granitic magmatism. The geochemistry data show that granites are high-potassium calcalkaline-shoshonite, peraluminous rock which is characterized by high silicon and aluminum, enriched alkali, low titanium, as well as enriched light rare earth elements (LREE) and large ion lithophile elements (LILE, e.g., K, Th and Rb), and depleted in high field-strength elements (HFSE, e.g., Nb, Ti, P, and Ta) with obvious Eu negative anomaly (the value of δEu is between 0.27 and 0.65). Halasen granites belong to highly fractionated Ⅰ-type granite. It is suggested that the Halasen granites were most likely derived from parental magma by mixing of depleted mantle-derived magma and induced crustal-melted felsic magma in the deep crust, and then suffered further differentiation during magma ascent. The subduction of the East Kunlun Paleo-Tethys Ocean lasted to the Early Triassic, and the Middle Triassic witnessed the intracontinental collision.
- granite,
- geochronology,
- geochemistry,
- Halasen,
- East Kunlun

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References(74)

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