东天山地区黄山东与香山镁铁质- 超镁铁质杂岩体对比

陈继平; 廖群安; 张雄华; 罗婷; 郭东宝; 胡兆初

doi:10.3799/dqkx.2013.117

Volume 38 Issue 6

Jun. 2013

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Article Navigation > Earth Science > 2013 > 38(6): 1183-1196

CHEN Ji-ping, LIAO Qun-an, ZHANG Xiong-hua, LUO Ting, GUO Dong-bao, HU Zhao-chu, 2013. Contrast of Huangshandong and Xiangshan Mafic-Ultramafic Complex, East Tianshan. Earth Science, 38(6): 1183-1196. doi: 10.3799/dqkx.2013.117

Citation:

CHEN Ji-ping, LIAO Qun-an, ZHANG Xiong-hua, LUO Ting, GUO Dong-bao, HU Zhao-chu, 2013. Contrast of Huangshandong and Xiangshan Mafic-Ultramafic Complex, East Tianshan. Earth Science, 38(6): 1183-1196. doi: 10.3799/dqkx.2013.117

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Contrast of Huangshandong and Xiangshan Mafic-Ultramafic Complex, East Tianshan

doi: 10.3799/dqkx.2013.117

1.
Shaanxi Center of Geological Survey, Xi'an 710016, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-12-01
Publish Date: 2013-06-01

Abstract

Abstract

Controlled by the NEE-trending Huangshan-Jingerquan ductile sheer zone, the Huangshandong and Xiangshan mafic-ultramafic complex belongs to the Huangshan-Jingerquan mafic-ultramafic rock belt located in the north of East-Tianshan. Huangshandong is characterized by being of calc-alkalic and tholeiitic series and being composed of pyroxene peridotite and gabbro, whereas Xiangshan mafic-ultramafic rocks are made up of pyroxene peridotite, olivine pyroxenite, hornblende gabbro and diabase, belonging to the tholeiitic series. Both rocks are enriched in large ion lithophile elements (such as K, Sr, Ba) and high field strength elements (such as Pb, U), depleted in high field strength elements (such as Nb, P) and slightly depleted in high field strength elements (such as Zr, Hf). However, they are different in the REE pattern, with Huangshandong showing the enrichment of LREE, similar to OIB features, while the Xiangshan rocks presenting the flat pattern of REE. They are the result of partial melting from the spinel source region and magma experienced olivine, pyroxene, plagioclase and amphibole. But they are subject to crust assimilation contamination to a different extent.Using the LA-ICP-MS method, we obtain the age of Huangshandong and Xiangshan at 277±1.1 Ma and 285±1.1 Ma respectively, which demonstrates they generated from the same tectonic setting, resulted from the lithospheric delamination at the root and the upwelling of asthenosphere in the partial melting of lithospheric mantle, corresponding to post-collision intermittent extension setting.
- mafic-ultramafic complex,
- Huangshandong,
- Xiangshan,
- zircon,
- magma source,
- post-collision extension,
- geochemistry

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References(80)

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