东昆仑马尼特地区片麻状花岗闪长岩锆石U-Pb年代学、地球化学及其构造背景

赵菲菲; 孙丰月; 刘金龙

doi:10.3799/dqkx.2017.073

Volume 42 Issue 6

Jun. 2017

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Article Navigation > Earth Science > 2017 > 42(6): 927-940

Zhao Feifei, Sun Fengyue, Liu Jinlong, 2017. Zircon U-Pb Geochronology and Geochemistry of the Gneissic Granodiorite in Manite Area from East Kunlun, with Implications for Geodynamic Setting. Earth Science, 42(6): 927-940. doi: 10.3799/dqkx.2017.073

Citation:

Zhao Feifei, Sun Fengyue, Liu Jinlong, 2017. Zircon U-Pb Geochronology and Geochemistry of the Gneissic Granodiorite in Manite Area from East Kunlun, with Implications for Geodynamic Setting. Earth Science, 42(6): 927-940. doi: 10.3799/dqkx.2017.073

Citation:

Zhao Feifei, Sun Fengyue, Liu Jinlong, 2017. Zircon U-Pb Geochronology and Geochemistry of the Gneissic Granodiorite in Manite Area from East Kunlun, with Implications for Geodynamic Setting. Earth Science, 42(6): 927-940. doi: 10.3799/dqkx.2017.073

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Zircon U-Pb Geochronology and Geochemistry of the Gneissic Granodiorite in Manite Area from East Kunlun, with Implications for Geodynamic Setting

doi: 10.3799/dqkx.2017.073

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

Received Date: 2016-11-02
Publish Date: 2017-06-15

Abstract

Abstract

In order to determine the formation time, magma source, and tectonic setting of the gneissic granodiorite in Manite area, East Kunlun, zircon U-Pb dating, Hf isotope data and geochemistry of the gneissic granodiorite are studied in this paper. The chronology indicates that the magmatic zircon LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry) U-Pb weighted mean age of the Manite gneissic granodiorite in the East Kunlun is 495.6±1.1 Ma (MSWD=0.13), belonging to the Late Cambrian. The gneissic granodiorites have SiO₂ of 61.47%-63.99%, Na₂O of 2.91%~3.64%, K₂O of 0.93%-2.31%, CaO of 4.29%-6.52%, ALK of 3.92%-5.69% and A/CNK=0.83~0.97. Chemically, they are metaluminous and belong to calc-alkaline rock series. The gneissic granodiorite is characterized by the enrichment of LILEs (Rb and K) and incompatible elements(Th and U), and depletion of HFSEs(Nb, Ta, Zr and Ti). The ratios of Nb/Ta, La/Nb, Th/Nb and Th/La show crustal characteristics. The ε_Hf(t) values of zircons from the gneissic granodiorite range from 12.2-15.0, their Hf two-stage model ages vary from 506 to 662 Ma. The initial materials are mainly derived from the juvenile crust. The gneissic granodiorite falls into the volcano arc granite area with the determination of trace elements in Rb-(Y+Nb) tectonic discrimination diagram and falls into the zone of pre-plate collision with the characteristics of active continental margin before the collision. Combined with the geochronological data, geochemical characteristics and the regional tectonic evolution, it is concluded that the gneissic granodiorite in the Manite area was formed in the environment of Proto-Tethys Ocean crust subduction, presumably it belongs to the southward subduction of oceanic crust. The crust between the Qaidam massif and Wanbaogou oceanic plateau occurred bidirectional subduction to the south and the north.
- gneissic granodiorite,
- geochemistry,
- zircon U-Pb dating,
- geochronology,
- Manite area,
- East Kunlun

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References(99)

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Zircon U-Pb Geochronology and Geochemistry of the Gneissic Granodiorite in Manite Area from East Kunlun, with Implications for Geodynamic Setting

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