2020 Vol. 26, No. 3
Article Contents

ZHANG Tao, CHEN Zhengle, HUANG Hongye, ZHANG Wengao, ZHANG Qing, PAN Jiayong, ZHOU Zhenju, ZOU Mingliang, FENG Hongye, WANG Xiaohu, HAN Fengbin, SUN Yue, HUO Hailong, MA Ji, YANG Bin. 2020. Geochemical characteristics of gold-bearing minerals and its geological significance in the Ashawayi gold deposit in the southwestern Tianshan Orogen. Journal of Geomechanics, 26(3): 443-458. doi: 10.12090/j.issn.1006-6616.2020.26.03.038
Citation: ZHANG Tao, CHEN Zhengle, HUANG Hongye, ZHANG Wengao, ZHANG Qing, PAN Jiayong, ZHOU Zhenju, ZOU Mingliang, FENG Hongye, WANG Xiaohu, HAN Fengbin, SUN Yue, HUO Hailong, MA Ji, YANG Bin. 2020. Geochemical characteristics of gold-bearing minerals and its geological significance in the Ashawayi gold deposit in the southwestern Tianshan Orogen. Journal of Geomechanics, 26(3): 443-458. doi: 10.12090/j.issn.1006-6616.2020.26.03.038

Geochemical characteristics of gold-bearing minerals and its geological significance in the Ashawayi gold deposit in the southwestern Tianshan Orogen

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  • Ashawayi gold deposit, the second largest gold deposit in the southwestern Tianshan Orogen, NW China, is located at the southern margin of the Central Asian Orogenic Belt of the "Asian Golden Belt". Detailed field observations showed that the regional area experienced two tectonic processes from early compression to lately strike-slip extension during the Paleozoic, and the mineralization was related to the transition from compression to extension. By the methods of mineragraphy, EMPA, SEM and S isotope analysis, the gold-bearing minerals in the ore deposit, the occurrence state of gold, the source of ore-forming materials, were determined in this paper, suggesting that gold-bearing minerals should be mainly composed of arsenian pyrite and some arsenopyrite. The formation of arsenic pyrite can be divided into three stages, i.e. sedimentary diagenesis stage (Py1), early ore-forming stage (Py2), and main ore-forming stage (Py3). The Py2 and Py3 are rich of As-Te, and deficit of S-Fe, while the content of S and As is significantly negatively correlated. The ratio value of Co/Ni indicates that the pyrite should be the origin of deposit-hydrothermal. The gold is mostly hosted in arsenic pyrite as the form of nano-scale "visible" natural gold (Au0). The δ34S value of pyrite and stibnite changes from 9.5‰ to 16.3‰, suggesting that the sulfur in ore-forming fluid should be a thermochemical reduction product of marine sulfate and ore-forming material probably resourced from the stratum. Therefore, the Ashawayi gold deposit should be a typical medium-shallow orogenic-type gold deposit, and the buried depth of ore-bodies is relatively shallow, suggesting a favorable prospecting potential in the deep.

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