ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
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
  
关键词:Miaowan Formation  black rock series  REE geochemistry  dry and anoxic environment  Northern Qinling
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)
作者单位E-mail
王立社 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 xawlishe@cgs.gov.cn 
侯俊富 西北大学地质系大陆动力学国家重点实验室  
张复新 西北大学地质系大陆动力学国家重点实验室  
秦艳 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  
曹红霞 西北大学地质系大陆动力学国家重点实验室  
齐亚林 中国石油天然气股份公司长庆油田研究院  
杨鹏飞 西安地质调查中心  
金拴联 中国石油天然气股份公司长庆油田研究院  
房波 中国石油天然气股份公司青海油田  
周燕 中国石油天然气股份公司青海油田  
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摘要:
REE Geochemical Characteristics of the Miaowan Formation Black Rock Series in North Qinling Mountain and Their Genetic Significance
      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 of w (V) /w (V +Ni)(= 0.38~0.93) are normal, and the ratios of w (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.
WANG Li-she,HOU Jun-fu,ZHANG Fu-xin,QIN Yan,CAO Hong-xia,QI Ya-lin,YANG Peng-fei,JIN Suan-lian,FANG Bo,ZHOU Yan.2010.REE Geochemical Characteristics of the Miaowan Formation Black Rock Series in North Qinling Mountain and Their Genetic Significance[J].Acta Geoscientica Sinica,31(1):73-82.
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