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《Geotectonica Et Metallogenia》 2007-02
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GEOLOGICAL AND GEOCHEMICAL CHARACTERISTICS OF HUOSHIBULAKE PB-ZN DEPOSIT IN XINJIANG

ZHANG Zhibin1,3, YE Lin1,2, LI Wenqian1, LI Chaoyang1, GAO Zhenquan2, LI Jianfeng1,3 and XU Lifeng1,3(1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, GZ 550002, China; 3. Graduate School of Chinese Academy of Sciences, Beijing 100049, China)  
The ore bodies and their hosting strata of Huoshibulake Pb-Zn deposit show consistent occurrence, and the ores of the main orebody are characterized by striped and laminar structures, in addition to well-developed organic textures such as framboidal spherules, tubular and zonal textures. All of these show that the ore deposit is strata-bound and of hydrothermal origin. The major elemental PER diagrams for samples of ores and ore-hosting rocks reveal that the ore-hosting carbonate rocks are mainly gypsiferous limestones with development of weak dolomitization, and that mineralization is intimately correlated to silicification. The ores, ore-hosting carbonate rocks and clastic rocks including shale, silt limestone and pelitic siltstone all show distinct trace elemental distribution patterns. Ore samples of the upper ore-body are enriched in transitional elements like Ti, V, Cr, Mn, Co and Ni, immobile elements like Zr and Hf, as well as large ion lithophile elements like Sr and Pb, but are depleted in mobile elements such as Na, K, Rb, Ba and immobile elements such as Nb, Th. Samples of recrystallized micritic limestones are enriched in transitional elements like Ti, Mn, Ni, large ion lithophile elements like Sr, Pb, depleted Zr, Hf, Nb, Th, and trace elements of the surrounding rocks for the lower ore-body. Samples of shales, silt limestones and pelitic siltstones distributed near the average upper crust line are obviously enriched in transitional elements like Ti, V, Cr, Mn, Co and Ni, large ion lithophile element Rb and immobile elements like Y, Zr, Hf, but are depleted in Na, Fe, Sr, Nb. All ore samples from the upper ore-body and part of the samples from the lower ore-body and its surrounding rocks are enriched in strong magmaphile elements like Cr, Co and Ni. The rare earth elemental distribution patterns for ore samples from the upper ore-body are characterized by strong positive europium anomaly, while samples from the wall rocks for the lower ore-body show clearly positive europium anomaly, which is lower than that for the upper ore-body. These geological and geochemical evidences support the conclusion that this deposit is a SEDEX-type hydrothermal deposit.
【Fund】: 国家重点基础研究发展规划项目(2001CB409805);; 中科院创新重要方向性项目(KZCX3-SW-137)资助
【CateGory Index】: P618.4
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