西天山伊什基里克山早石炭世火山岩浆作用及其成矿

李永军; 胡克亮; 周继兵; 佟丽莉; 佟黎明

doi:10.3799/dqkx.2010.023

Volume 35 Issue 2

Mar. 2010

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Article Navigation > Earth Science > 2010 > 35(2): 235-244

LI Yong-jun, HU Ke-liang, ZHOU Ji-bing, TONG Li-li, TONG Li-ming, 2010. Early Carboniferous Volcano-Magmatism and Related Mineralization in Yishijilike Mountain, Western Tianshan. Earth Science, 35(2): 235-244. doi: 10.3799/dqkx.2010.023

Citation:

LI Yong-jun, HU Ke-liang, ZHOU Ji-bing, TONG Li-li, TONG Li-ming, 2010. Early Carboniferous Volcano-Magmatism and Related Mineralization in Yishijilike Mountain, Western Tianshan. Earth Science, 35(2): 235-244. doi: 10.3799/dqkx.2010.023

Citation:

LI Yong-jun, HU Ke-liang, ZHOU Ji-bing, TONG Li-li, TONG Li-ming, 2010. Early Carboniferous Volcano-Magmatism and Related Mineralization in Yishijilike Mountain, Western Tianshan. Earth Science, 35(2): 235-244. doi: 10.3799/dqkx.2010.023

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Early Carboniferous Volcano-Magmatism and Related Mineralization in Yishijilike Mountain, Western Tianshan

doi: 10.3799/dqkx.2010.023

1.
College of Earth Science and Resources, Chang'an University, Xi'an 710054, China
2.
Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China
3.
Xinjiang Bureau of Geology and Mineral Exploration and Developnent, Urumqi 830000, China

Received Date: 2008-09-25
Publish Date: 2010-03-01

Abstract

Abstract

The volcanic rock assemblage of Dahalajunshan Formation is island arc calc-alkaline sodic volcanic rocks formed at plate convergent margins. The distribution of the volcanic rocks coincides with the anomaly of Au-Cu. All the gold-copper ore spots and mineralization spots in this area are volcanic rock-hosted of Dahalajunshan volcanic rocks,which show favorable ore-forming condition of gold-copper deposits. The gold mineralization is hosted in volcanic rocks mostly,and the epithermal gold deposit is the most significant type in this region. The Kulesayi porphyry is calc-alkaline hypabyssal rock,whose average SiO₂ is 57.06%-70.74%,and they are rich in Al₂O₃,Na₂O,Sr and LREE,poor in MgO,Y,Yb and very poor in HREE. With their Na₂O/K₂O of more than 1,Sr/Y of 57.67,and positive anomaly of Eu,they have characters of O-type adakite. The Kulesayi porphyry coincides with anomaly of Mo. Molybedenun deposit with good prospects for further exploration has been found here. The Kulesayi porphyry and Dahalajunshan volcanic rocks compose the assemblage of island arc volcanic rocks in Early Carboniferous,which enriches the tectonic rock association in this region,and is important for the geotectonic evolution study,regional metallogenic law exploration,and prospecting for the gold-copper deposit (relative to island arc volcanic rocks) and copper-molybedenun deposit (relative to adakite).
- Early Carboniferous,
- calc-alkaline island arc volcanic rock,
- adakite,
- gold-copper-molybedenun mineralization,
- Yishijilike Mountain,
- western Tianshan

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Early Carboniferous Volcano-Magmatism and Related Mineralization in Yishijilike Mountain, Western Tianshan

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