| 北秦岭庙湾组黑色岩系稀土元素地球化学特征及成因意义 |
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| 引用本文： | 王立社,侯俊富,张复新,秦艳,曹红霞,齐亚林,杨鹏飞,金拴联,房波,周燕.北秦岭庙湾组黑色岩系稀土元素地球化学特征及成因意义[J].地球学报,2010,31(1):73-82. |
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| 作者姓名： | 王立社 侯俊富 张复新 秦艳 曹红霞 齐亚林 杨鹏飞 金拴联 房波 周燕 |
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| 作者单位： | 西安地质调查中心,西北大学地质系大陆动力学国家重点实验室;西北大学地质系大陆动力学国家重点实验室;西北大学地质系大陆动力学国家重点实验室;中国科学院广州地球化学研究所有机地球化学国家重点实验室;西北大学地质系大陆动力学国家重点实验室;中国石油天然气股份公司长庆油田研究院;西安地质调查中心;中国石油天然气股份公司长庆油田研究院;中国石油天然气股份公司青海油田;中国石油天然气股份公司青海油田 |
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| 基金项目： | 西北有色地勘局地勘院“陕西南部黑色岩系金属矿床成矿规律及找矿预测研究”(编号: 地勘[2006])和中国地质调查局“昆仑-阿尔金成矿带地质矿产调查综合研究”(编号: 1212010913015) |
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| 摘 要： | 笔者采用等离子质谱仪(ICP-MS)方法对北秦岭大荆区奥陶纪—志留纪庙湾组黑色岩系岩石的稀土元素及V、Ni、Cr、U、Th等微量元素含量进行了测定。结果显示岩石轻稀土元素相对重稀土元素富集, Eu异常值δEu为0.63~10.61(绝多数大于1.54)多呈正异常, Ce异常值δCe为0.65~1.02(平均为0.893) 异常微弱且有正负差异; U/Th值为0.38~4.07, w (V)/w (V +Ni)值为0.38~0.93以及w (Ce)/w (La)值为1.27~2.17。将这些特征值与前人研究成果对比, 并利用La/Yb-Ce/La和La/Yb-REE判别图解判别后, 认为北秦岭区庙湾组黑色岩系形成于活动陆缘一种干燥缺氧较深浅海环境, 黑色岩系形成过程中有热液作用参与。
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| 关 键 词： | 庙湾组 黑色岩系 稀土地球化学 干燥缺氧环境 北秦岭 |
REE Geochemical Characteristics of the Miaowan Formation Black Rock Series in North Qinling Mountain and Their Genetic Significance |
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| WANG Li-she,HOU Jun-fu,ZHANG Fu-xin,QIN Yan,CAO Hong-xi,QI Ya-lin,YANG Peng-fei,JIN Suan-lian,FANG Bo and ZHOU Yan.REE Geochemical Characteristics of the Miaowan Formation Black Rock Series in North Qinling Mountain and Their Genetic Significance[J].Acta Geoscientia Sinica,2010,31(1):73-82. |
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| Authors: | WANG Li-she HOU Jun-fu ZHANG Fu-xin QIN Yan CAO Hong-xi QI Ya-lin YANG Peng-fei JIN Suan-lian FANG Bo and ZHOU Yan |
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| Abstract: | The abundances of rare earth elements and some trace elements such as V, Ni, Cr, U and Th of the black rock series from the Miaowan Formation in North Qinling Mountain were measured by using the ICP-MS method.The results show that the black rock series of the Miaowan Formation is usually of the LREE-enriched type, that the samples are characterized by slightly negative or positive Ce anomalies (δCe=0.65～1.02) and distinct positive Eu anomalies (with δEu mostly higher than 1.54), and that the ratios of U/Th display a wide variation range from 0.38 to 4.07, the ratios ofw (V)/w (V +Ni)(=0.38～0.93) are normal, and the ratios ofw (Ce)/w (La) (=1.27～2.17) are relatively high. A study of the parameters of REE and trace elements in comparison with the available data and an analysis of the La/Yb-Ce/La and La/Yb- REE diagrams reveal that the black rock series was formed in a dry, anoxic and shallow sea environment belonging to an active continental margin, with the participation of some hydrothermal fluids. |
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| Keywords: | Miaowan Formation black rock series REE geochemistry dry and anoxic environment Northern Qinling |
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