柴北缘大柴旦滩间山花岗斑岩体锆石U-Pb年代学、地球化学及Hf同位素

张延军; 孙丰月; 许成瀚; 禹禄

doi:10.3799/dqkx.2016.127

Volume 41 Issue 11

Nov. 2016

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Article Navigation > Earth Science > 2016 > 41(11): 1830-1844

Zhang Yanjun, Sun Fengyue, Xu Chenghan, Yu Lu, 2016. Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China. Earth Science, 41(11): 1830-1844. doi: 10.3799/dqkx.2016.127

Citation:

Zhang Yanjun, Sun Fengyue, Xu Chenghan, Yu Lu, 2016. Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China. Earth Science, 41(11): 1830-1844. doi: 10.3799/dqkx.2016.127

Citation:

Zhang Yanjun, Sun Fengyue, Xu Chenghan, Yu Lu, 2016. Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China. Earth Science, 41(11): 1830-1844. doi: 10.3799/dqkx.2016.127

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Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China

doi: 10.3799/dqkx.2016.127

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

Received Date: 2016-04-25
Publish Date: 2016-11-15

Abstract

Abstract

In order to research the Variscan tectonic evolution features of Dachaidan region in North Qaidam, this paper presents LA-ICP-MS zircon U-Pb dating, geochemical and Hf isotopic data of the granite porphyry from Tanjianshan intrusion in Dachaidan region, with the aim of constraining its formation time, petrogenesis and the regional tectonic setting. The LA-ICP-MS U-Pb dating results of zircons from the granite porphyry indicate that the intrusion formed in the Late Devonian Epoch (356.0±2.8 Ma, MSWD=0.53). Geochemically, these rocks fall into the calc-alkaline to middle-K calc-alkaline series, with an A/CNK ratio of 0.97-1.10, which are weakly peraluminous granites, being of the characteristics of I type granitoids, enriched 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 granite porphyry vary from ±5.43 to ±8.38, and two-stage model ages (T_DM2) range from 1 017 to 1 284 Ma. These characteristics suggest that the primary magma was derived from the remelting of juvenile crustal materials in Mesoproterozoic. In context of its regional geological background, we conclude the granite porphyry from Tanjianshan intrusion were formed extensional tectonic setting after the collision between Qaidam block and Qilian block.
- zircon U-Pb chronology,
- Zircon Hf isotopes,
- Tanjianshan,
- geochemistry,
- geochronology

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References(131)

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Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China

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