WANG Hong, LI Zhi-ming, BAO Qing-zhong, SHA De-ming, HU Xiu-jun. The primary study of the geological characteristics and origin for Chahansala Sb Deposit[J]. Northwestern Geology, 2003, 36(2): 66-71.
Citation: |
WANG Hong, LI Zhi-ming, BAO Qing-zhong, SHA De-ming, HU Xiu-jun. The primary study of the geological characteristics and origin for Chahansala Sb Deposit[J]. Northwestern Geology, 2003, 36(2): 66-71.
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The primary study of the geological characteristics and origin for Chahansala Sb Deposit
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1.
Institude of Resourcers and Civil Engineering, Northeast University, Shenyang 110004, China;Shenyang Institude of Geology and Mineral Resources, Shenyang 110033, China
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2.
Xi'an Institude of Geology and Mineral Resources, Xi'an 710054, China
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3.
No 3 Geological Party, Xinjiang Bureau of Geology and Exploration, Korla 841000, China
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Abstract
Chahansala Sb deposit is located in the centre section of southwestern Tianshan which belongs to the western part of Late Paleozoic trench-arc zone in Xinjiang.And it constitutes the Chahansala Sb-Au deposit zone with the Shawayaer dun Au-Sb-Ag deposit the Kalajiaoguya Sb-Au deposit, and the Gulekedabankati Sb-Au deposit.The mineral district sits on the concentrated centre of the Chahansala Sb abnormal area and controlled by a huge thrusting nappestructure.The ore bodies are in the carbon-bearing fragmental rock of the Aertengkeshi formation, and demonstrate the character of multi-element and multi-stage mineralization.The minerogenic material is from the formation that contains the ore bodies, and the minerogenic hydrotherm is the mixed solution that contains the magmatic water, meteoric water, and metamorphic water.
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