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《Mineral Deposits》 2015-01
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Geochemistry of volcanic and intrusive rocks in Zhibo iron ore deposit of western Tianshan Mountains

TIAN JingQuan;DUAN ShiGang;PENG WanLin;LI Ming;JIANG ZongSheng;YAN Rui;Faculty of Earth Resources, China University of Geosciences;No. 3 Geological Party,Xinjiang Bureau of Geology and Mineral Resources;MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;  
A number of large and medium-sized submarine volcanics-hosted iron-rich ore deposits were discovered recently in the Awulale Mountain, western Tianshan Mountains. These iron ore deposits are considered to be genetically related to volcanism. However, the tectonic setting for the volcanism and iron mineralization remains uncluear. The Zhibo iron ore deposit is hosted in basalts and andesites of the Lower Carboniferous Dahalajunshan Formation. The volcanic rocks were intruded by Late Carboniferous granite, granitic dykes and dioritic dykes. Samples of basalt and andesite fall in volcanic arc region in the tectonic discrimination diagrams, whereas samples of granite, granitic dykes and dioritic dykes fall in volcanic arc and / or syn-collision environment in the tectonic discrimination diagram for granitoids. Combined with previous researches, this paper argues for an island arc setting in Early Carboniferous and a transition from island arc to collision in Late Carboniferous for the Zhibo deposit. Basalt samples are depleted in Ta and Nb, relatively depleted in Th, but eniched in Rb, U and Pb. Andesite samples are depleted in Ta and Nb, but enriched in light REE and Rb, U, Th and Pb. Combined with Sr / Th versus Th / Ce and Th versus Ba / Th diagrams and other geochemical data, the authors hold that the magma source for basalt and andesite was mantle wedge metasomatized by subduction-related aqueous fluids.
【Fund】: 国家重点基础研究发展计划(编号:2012CB416803);; 地质矿产调查评价项目(编号:1212011085060、1212011090300);; 国家自然科学基金资助项目(编号:41203035)联合资助
【CateGory Index】: P618.31;P588.1
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