东昆仑按纳格角闪辉长岩体地球化学特征及其对古特提斯洋演化的制约

赵旭; 付乐兵; 魏俊浩; 赵玉京; 唐洋; 杨宝荣; 管波; 王晓云

doi:10.3799/dqkx.2018.020

Volume 43 Issue 2

Feb. 2018

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Article Navigation > Earth Science > 2018 > 43(2): 354-370

Zhao Xu, Fu Lebing, Wei Junhao, Zhao Yujing, Tang Yang, Yang Baorong, Guan Bo, Wang Xiaoyun, 2018. Geochemical Characteristics of An'nage Hornblende Gabbro from East Kunlun Orogenic Belt and Its Constraints on Evolution of Paleo-Tethys Ocean. Earth Science, 43(2): 354-370. doi: 10.3799/dqkx.2018.020

Citation:

Zhao Xu, Fu Lebing, Wei Junhao, Zhao Yujing, Tang Yang, Yang Baorong, Guan Bo, Wang Xiaoyun, 2018. Geochemical Characteristics of An'nage Hornblende Gabbro from East Kunlun Orogenic Belt and Its Constraints on Evolution of Paleo-Tethys Ocean. Earth Science, 43(2): 354-370. doi: 10.3799/dqkx.2018.020

Citation:

Zhao Xu, Fu Lebing, Wei Junhao, Zhao Yujing, Tang Yang, Yang Baorong, Guan Bo, Wang Xiaoyun, 2018. Geochemical Characteristics of An'nage Hornblende Gabbro from East Kunlun Orogenic Belt and Its Constraints on Evolution of Paleo-Tethys Ocean. Earth Science, 43(2): 354-370. doi: 10.3799/dqkx.2018.020

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Geochemical Characteristics of An'nage Hornblende Gabbro from East Kunlun Orogenic Belt and Its Constraints on Evolution of Paleo-Tethys Ocean

doi: 10.3799/dqkx.2018.020

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Qinghai Bureau of Nonferrous Metals Geology and Mineral Exploration, Xining 810007, China

Received Date: 2017-07-08
Publish Date: 2018-02-15

Abstract

Abstract

At present, the research on Permian-Triassic basic magmatic rocks in East Kunlun orogenic belt is extremely weak, which not only limits the understanding of the nature of the mantle source in the study area during this period but also restricts the accurate understanding of the evolution processes of Paleo-Tethys Ocean.The zircon LA-ICP-MS U-Pb geochronology and major and trace elements, as well as Sr-Nd-Hf isotope geochemistry of the An'nage hornblende gabbro in the East Kunlun orogenic belt are applied in this paper.LA-ICP-MS zircon U-Pb dating yields a weighted mean age of 242±2 Ma for the intrusion.It is characterized by low SiO₂(46.00%-52.40%), low(Na₂O+K₂O)(3.07%-3.79%) contents.In addition, it is enriched in Al₂O₃(17.35%-20.10%), MgO(4.65%-6.53%) and FeO^T(8.77%-11.07%) with high Mg^#(68-75), indicating that it belongs to the calc-alkaline series.This intrusion has low(La/Yb)_N and Nb/Ta ratios, negative Eu anomalies, with enriched large-ion lithophile elements and depleted high field strength elements.All geochemical characteristics show that this intrusion is the result of typical island arc magmatic activity.Additionally, the samples have relatively uniform(⁸⁷Sr/⁸⁶Sr)_i ratios(0.708 80-0.710 36) and ε_Nd(t) values(-4.8 to -3.4), and relatively high ε_Hf(t) values(-4.9 to -0.4).According to the lithology, geochemical characteristics and isotopic compositions of the intrusion, we propose that the magma has not been significantly contaminated by the crust and it was derived from the low-degree partial melting(2%-10%) of the mantle wedge, which had undergone metasomatism induced by the fluid from the subducted slab.The mantle source was characterized by the spinel phase-phlogopite lherzolite.Slight fractional crystallization of pyroxene and plagioclase might also occur during the evolution of magma.In combination with the tectonic evolution of the East Kunlun orogenic belt and the geochronological and geochemical characteristics of contemporary intrusive rocks, it is concluded that the An'nage hornblende gabbro was produced at the late stage of Paleo-Tethys Ocean subduction, and the final closure timing of Paleo-Tethys Ocean should be the Middle Triassic to Late Triassic.
- hornblende gabbro,
- Triassic,
- Paleo-Tethys Ocean,
- subduction,
- East Kunlun orogenic belt,
- geochronology,
- geochemistry

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References(95)

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