吉林延边地区棉田岩体锆石U-Pb年代学、地球化学及Hf同位素

刘金龙; 孙丰月; 林博磊; 王英德; 王硕; 胡安新

doi:10.3799/dqkx.2015.004

Volume 40 Issue 1

Jan. 2015

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Article Navigation > Earth Science > 2015 > 40(1): 49-60

Liu Jinlong, Sun Fengyue, Lin Bolei, Wang Yingde, Wang Shuo, Hu Anxin, 2015. Geochronology, Geochemistry and Zircon Hf Isotope of Miantian Granodiorite Intrusion in Yanbian Region, Southern Jinlin Province and Its Geological Significance. Earth Science, 40(1): 49-60. doi: 10.3799/dqkx.2015.004

Citation:

Liu Jinlong, Sun Fengyue, Lin Bolei, Wang Yingde, Wang Shuo, Hu Anxin, 2015. Geochronology, Geochemistry and Zircon Hf Isotope of Miantian Granodiorite Intrusion in Yanbian Region, Southern Jinlin Province and Its Geological Significance. Earth Science, 40(1): 49-60. doi: 10.3799/dqkx.2015.004

Citation:

Liu Jinlong, Sun Fengyue, Lin Bolei, Wang Yingde, Wang Shuo, Hu Anxin, 2015. Geochronology, Geochemistry and Zircon Hf Isotope of Miantian Granodiorite Intrusion in Yanbian Region, Southern Jinlin Province and Its Geological Significance. Earth Science, 40(1): 49-60. doi: 10.3799/dqkx.2015.004

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Geochronology, Geochemistry and Zircon Hf Isotope of Miantian Granodiorite Intrusion in Yanbian Region, Southern Jinlin Province and Its Geological Significance

doi: 10.3799/dqkx.2015.004

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Information Center of Ministry of Land and Resources of People's Republic of China, Beijing 100812, China

Received Date: 2014-03-10
Publish Date: 2015-01-15

Abstract

Abstract

This paper presents LA-ICP-MS zircon U-Pb dating, geochemical and Hf isotopic data of the granodiorite from Miantian intrusion in Yanbian region, with the aim of constraining its petrogenesis and beginning time of subduction of the Paleo-Pacific plate beneath the Eurasian continent. The Miantian intrusion consists mainly of granodiorite with minor diorite. The LA-ICP-MS U-Pb dating results of zircons from the granodiorite indicate that the intrusion formed in the Early Jurassic (177±2 Ma, MSWD=1.13). Geochemically, these rocks fall into the calc-alkaline to high-K calc-alkaline series, with A/CNK ratios of 0.88-1.12, which are sub-aluminous granites, being of the characteristics of I type granitoids, enrichment in LILE (such as K, Ba, Rb), LREE, Th and U, relatively depleted in HFSE (such as Ta, Nb, Ti, P). The ε_Hf(t) values of the granodiorite vary from ±8.72 to ±12.28, and two-stage model ages (T_DM2) vary from 437 to 663 Ma. These characteristics suggest that the primary magma was derived from the remelting of juvenile crustal materials (Neoproterozoic to Early Paleozoic). It is concluded that granodiorite from Miantian intrusion formed in compressional structure setting similar to volcanic arc which could be related to the subduction of the Paleo-Pacific plate beneath the Eurasian continent.
- zircon U-Pb chronology,
- zircon Hf isotope,
- geochemistry,
- Yanbian

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References(91)

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