青海阿尼玛卿蛇绿混杂岩带西段哥日卓托杂岩体年代学、地球化学及Hf同位素

刘金龙; 孙丰月; 李良; 赵菲菲; 王英德; 王硕; 张宇婷

doi:10.3799/dqkx.2015.081

Volume 40 Issue 6

Jun. 2015

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Article Navigation > Earth Science > 2015 > 40(6): 965-981

Liu Jinlong, Sun Fengyue, Li liang, Zhao Feifei, Wang Yingde, Wang Shuo, Zhang Yuting, 2015. Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone. Earth Science, 40(6): 965-981. doi: 10.3799/dqkx.2015.081

Citation:

Liu Jinlong, Sun Fengyue, Li liang, Zhao Feifei, Wang Yingde, Wang Shuo, Zhang Yuting, 2015. Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone. Earth Science, 40(6): 965-981. doi: 10.3799/dqkx.2015.081

Citation:

Liu Jinlong, Sun Fengyue, Li liang, Zhao Feifei, Wang Yingde, Wang Shuo, Zhang Yuting, 2015. Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone. Earth Science, 40(6): 965-981. doi: 10.3799/dqkx.2015.081

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Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone

doi: 10.3799/dqkx.2015.081

College of Earth Sciences, Jilin University, Changchun 130061, China

Received Date: 2014-09-15
Publish Date: 2015-06-15

Abstract

Abstract

The Gerizhuotuo complex intrusion, a typical 'stitching pluton' with its long axis cutting regional structural lines, is significant in tectonic geochronology for providing an upper-age for the timing of plate collision. The zircon U-Pb dating results indicate that the pluton was formed in 227-224 Ma. Geochemically, porphyritic granite falls into the high-K calc-alkaline series, with high Sr(479-573 μg/g) and low Yb(1.03-1.20 μg/g) and Mg^#(48.7-51.8), being of the characteristics of adakitic rocks. The in situ zircon ε_Hf(t) value varies from -2.40 to 2.98, which suggests that the primary magma was derived from partial melting of lower crustal materials. Diorite also shows high-K calc-alkaline affinitie, with a Ti/Yb ratio ranging from 1 930 to 2 178, Nb/Ta ratio ranging from 15.9 to 17.4. It is suggested that a mixture, between basaltic magma derived from partial melting of metasomatized mantle and acidic magma derived from crustal material, produced the dioritic magma. It is concluded that the pluton was formed in a post-collisional tensional environment.
- zircon U-Pb age,
- zircon Hf isotope,
- adakiteic rock,
- geochemistry,
- geochronology

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References(109)

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Geochronology, Geochemistry and Hf Isotopes of Gerizhuotuo Complex Intrusion in West of Anyemaqen Suture Zone

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