青海省沱沱河地区楚多曲铅锌矿床流体包裹体特征及矿床成因探讨 |
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引用本文: | 邹公明,;李世金,;李良,;钱烨,;李连松.青海省沱沱河地区楚多曲铅锌矿床流体包裹体特征及矿床成因探讨[J].西北地质,2014(4):256-263. |
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作者姓名: | 邹公明 ;李世金 ;李良 ;钱烨 ;李连松 |
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作者单位: | [1]青海省第三地质矿产勘查院,青海西宁810029; [2]青海省地质调查局,青海西宁810001; [3]吉林大学地球科学学院,吉林长春130061; [4]青海省第五地质矿产勘查院,青海西宁810028 |
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基金项目: | 青海省地勘基金项目“青海省沱沱河地区成矿规律及找矿方向研究”(青国土资矿[2011]214号,[2012]28号) |
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摘 要: | 青海省沱沱河地区楚多曲铅锌矿为近年来发现的一处大型铅锌矿床。铅锌矿体主要呈脉状产出,主要受控于切割碳酸盐岩地层的陡倾断裂。通过对系统流体包裹体研究,结果表明,石英中流体包裹体较为发育,主要为气液两相包裹体。成矿流体均一温度为160~220℃,盐度w(NaCl)为8%~10%,密度为0.90~0.95g/cm3,具有低温、低盐度、低密度的特征。估算成矿压力为11~13MPa,深度为1.1~1.3km,属浅成深度。成矿流体δD为-96.4‰~122.1‰,δ18 OH2O值为2.1‰~9.5‰。综合区域构造背景、铅锌矿体形成特点、流体包裹体特征及矿石组构等相关信息,认为楚多曲铅锌矿矿床成因类型为受断裂控制的中低温热液脉型铅锌矿床。该认识可极大拓展青海省沱沱河地区铅锌矿的找矿潜力,具有重要的研究意义和实用价值。
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关 键 词: | 流体包裹体 矿床成因 中低温热液脉型 楚多曲铅锌矿床 沱沱河地区 |
Characteristics of Fluid Inclusions and Ore Genesis of Chuduoqu Pb-Zn Ore Deposit in Tuotuohe Area,Qinghai Province |
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Institution: | ZOU Gong-ming , LI Shi-jin , LI Liang , QIAN Ye , LI Lian-song (1. The No. 3 Institute of Geology and Minerals Exploration of Qinghai Province, Xining 810029, China ; 2. Qinghai Bureau of Geological Survey, Xining 810001, China; 3. College of Earth Sciences, Jilin University, Changchun 130061, China; 4. The No. 5 Institute of Geology and Minerals Exploration of Qinghai Province, Xining 810028, China) |
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Abstract: | The Chuduoqu Pb-Zn deposit is a large newly found mineral deposit in Tuotuohe of Qinghai Province. Its ore-bodies occur as veins, controlled by the steep fracture that cut the car- bonatite strata. The research of fluid inclusion shows that fluid inclusions are well developed in quartz, mainly in gas-liquid phase. The ore-forming fluid is characterized by medium-low temper- ature (160-220℃), low salinity (8%-10%NAC1) and low density (0.90-0.95 g/cm3), with pres- sure of 11 to 13 MPa and depth of 1.1 to 1.3 km. The 3D value of the ore-forming fluid is - 122. 1%0 to -96.4%0 and the 318OH20 value is 2.1%0 to 9.5%0. Combined with the regional tecton- ic background, ore-forming characteristics of lead and zinc, fluid inclusions and ore fabrics, this paper summarized that Chuduoqu Pb-Zn deposit is a medium-low temperature hydrothermal vein Pb-Zn deposit controlled by fractures. This conclusion is of great academic and applied signifi- cance to improve lead-zinc ore potential in Tuotuohe area. |
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Keywords: | fluid inclusions genesis of deposit medium-low temperature hydrothermal veintype Chuduoqu Pb-Zn deposit Tuotuohe area |
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