| 豫西骆驼山多金属硫铁矿床硫化物Rb-Sr等时线年龄及其地质意义 |
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| 引用本文： | 杨晨英,叶会寿,向君峰,陈小丹,邢波,李亮,王赛.豫西骆驼山多金属硫铁矿床硫化物Rb-Sr等时线年龄及其地质意义[J].矿床地质,2016,35(3):573-590. |
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| 作者姓名： | 杨晨英 叶会寿 向君峰 陈小丹 邢波 李亮 王赛 |
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| 作者单位： | 1. 中国地质大学地球科学与资源学院,北京,100083;2. 中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室,北京,100037;3. 昆明理工大学国土资源工程学院,云南 昆明,650093 |
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| 基金项目： | 本文得到国家科技支撑计划项目(编号:2011BAB04B06)、国家自然科学基金(编号:41303233、41403041)和国土资源部公益性行业基金(编号:200911007-08)联合资助 |
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| 摘 要： | 豫西骆驼山多金属硫铁矿床位于华北陆块南缘南泥湖矿田西北侧。为确定该矿床的形成时代,文章选取了8件硫化物矿物样品,采用Rb_Sr等时线定年方法测定成矿年龄。结果获得,闪锌矿+磁黄铁矿+方铅矿等时线年龄为(137.3±2.6)Ma,闪锌矿+方铅矿等时线年龄为(138.2±5.8)Ma,闪锌矿+磁黄铁矿等时线年龄为(137±3)Ma,磁黄铁矿+方铅矿等时线年龄为(137.1±2.7)Ma,方铅矿等时线年龄为(138.4±7.6)Ma,磁黄铁矿等时线年龄为(137.2±3.7)Ma。上述定年结果表明,骆驼山多金属硫铁矿床的成矿时代为137 Ma左右,属早白垩世。硫化物Sr同位素初始比值(~(87)Sr/~(86)Sr)i介于0.713 23~0.713 32,平均值为0.713 25,小于陆源硅酸盐Sr的初始值0.7190,而高于地幔Sr的初始值0.7040,表明成矿物质来源于壳幔混合。骆驼山多金属硫铁矿床与矿田内的南泥湖_三道庄斑岩_矽卡岩钼(钨)矿床、冷水北沟铅锌矿成矿时代基本一致,是同一构造_岩浆_流体成矿活动的产物。结合前人对华北陆块南缘中生代期间地球动力学背景研究成果,笔者认为骆驼山矿床是中国东部中生代构造体制大转折过程晚期的产物。
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| 关 键 词： | 地球化学 Rb-Sr等时线年龄 成矿时代 闪锌矿 骆驼山多金属硫铁矿床 豫西 |
| 收稿时间： | 2015/6/12 0:00:00 |
| 修稿时间： | 2016/2/19 0:00:00 |
Rb-Sr isochron age of sulfide minerals in Luotuoshan pyrite-polymetallic deposit of western Henan Province and its geological significance |
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| YANG ChenYing,YE HuiShou,XIANG JunFeng,CHEN XiaoDan,XING Bo,LI Liang and WANG Sai.Rb-Sr isochron age of sulfide minerals in Luotuoshan pyrite-polymetallic deposit of western Henan Province and its geological significance[J].Mineral Deposits,2016,35(3):573-590. |
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| Authors: | YANG ChenYing YE HuiShou XIANG JunFeng CHEN XiaoDan XING Bo LI Liang and WANG Sai |
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| Institution: | School of Earth Science and Resources, China University of Geolosciences, Beijing 100083, China,MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China,MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China,MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China,School of Earth Science and Resources, China University of Geolosciences, Beijing 100083, China,College of Land Resources Engineering, Kunming University of Technology, Kunming 650093, Yunnnan, China and School of Earth Science and Resources, China University of Geolosciences, Beijing 100083, China |
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| Abstract: | The Luotuoshan pyrite-polymetallic deposit lies on the northwestern side of the Nannihu orefield which is located on the southern margin of the North China craton. In order to determine the metallogenic age of the deposit, the authors chose eight sulfide mineral samples to determine the metallogenic age by using the Rb-Sr isochron dating method. The result shows that the isochron age of sphalerite+pyrrhotite+galena, sphalerite+galena, sphalerite+pyrrhotite, pyrrhotite+galena, sphalerite and pyrrhotite are (137.3±2.6) Ma, (138.2±5.8) Ma, (137±3) Ma, (137.1±2.7) Ma, (138.4±7.6) Ma and (137.2±3.7) Ma, respectively. These dating results indicate that the metallogenic age of the Luotuoshan pyrite-polymetallic deposit is about 137 Ma, suggesting Early Cretaceous. The (87Sr/86Sr)i of sulfides range from 0.71323 to 0.71332, with an average of 0.71325, lower than the (87Sr/86Sr)i ratio of the terrigenous silicates (0.7190) and higher than that of the mantle (0.7040), implying that the ore-forming materials were derived from the crust-mantle mixture. The Luotuoshan pyrite-polymetallic deposit has basically the same metallogenic age as the Nannihu-Sandaozhuang porphyry-skarn molybdenum (tungsten) deposit and the Lengshuibeigou lead-zinc deposit. They are the products of the same structure-magma-ore-forming-fluid activities. Combined with the previous studies of the geodynamic settings of the East Qinling orogenic belt during the Mesozoic period, it is held that the Luotuoshan pyrite-polymetallic deposit is the product of great transition period of late Mesozoic tectonic regime in eastern China. |
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| Keywords: | geochemistry Rb-Sr isochron age metallogenic age sphalerite Luotuoshan pyrite-polymetallic deposit western Henan Province |
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