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内蒙古白云鄂博地区新元古界温都尔庙群洋壳残片特征及地质意义
引用本文:王继春,肖荣阁,苏士杰,廖蕾,刘少华,梁锋.内蒙古白云鄂博地区新元古界温都尔庙群洋壳残片特征及地质意义[J].地质找矿论丛,2011,26(1):51-57.
作者姓名:王继春  肖荣阁  苏士杰  廖蕾  刘少华  梁锋
作者单位:王继春,WANG Ji-chun(中国地质大学(北京)地球科学与资源学院,北京,100083;内蒙古自治区地质调查院,呼和浩特,010022);肖荣阁,刘少华,XIAO Rong-ge,LIU Shao-hua(中国地质大学(北京)地球科学与资源学院,北京,100083);苏士杰,SU Shi-jie(内蒙古自治区地质调查院,呼和浩特,010022);廖蕾,LIAO Lei(内蒙古自治区地质勘查基金管理中心,呼和浩特,010022);梁锋,LIANG Feng(中钢集团天津地质研究院,天津,300061)
基金项目:中国地质调查局国土资源大调查项目
摘    要:文章从温都尔庙群岩石组合、岩石化学和同位素年龄特征入手,研究显示该套岩石具有洋中脊拉斑玄武岩的特征;岩石稀土特征表明其形成于陆间小洋盆环境.它属于华北板块北缘中段新元古代构造演化阶段的产物,为研究华北板块北缘地壳演化提供了新的依据.

关 键 词:温都尔庙群  洋壳残片  新元古代  华北板块  白云鄂博  内蒙古
收稿时间:2010/5/4 0:00:00

Characteristics and geological significance of oceanic crust relics in Neo-proterozoic Ondorsum group in Baiyun'ebo area,Inner Mongolia
WANG Ji-chun,XIAO Rong-ge,SU Shi-jie,LIAO Lei,LIU Shao-hua and LIANG Feng.Characteristics and geological significance of oceanic crust relics in Neo-proterozoic Ondorsum group in Baiyun'ebo area,Inner Mongolia[J].Contributions to Geology and Mineral Resources Research,2011,26(1):51-57.
Authors:WANG Ji-chun  XIAO Rong-ge  SU Shi-jie  LIAO Lei  LIU Shao-hua and LIANG Feng
Institution:WANG Ji-chun1,2,XIAO Rong-ge1,SU Shi-jie2,LIAO Lei3,LIU Shao-hua1,LIANG Feng4(1.Faculty of Earth Sciences and Mineral Resources,China University of Geosciences,Beijing 100083,China,2.Geological Survey Institute of Inner Mongolia,Hohhot 010022,3.Center for Fund of Geological Prospect of Inner Mongolia,4.Sinosteel Tianjin Geological Academy,Tianjin 300061,China)
Abstract:Study on rock assemblage,petrochemistry and isotopic age of Ondorsum Group shows that this rock assemblage is characteristic of ORB and the REE pattern reflects a small inter-continent basin sedimentary environment.The assemblage is the product of Neo-proterozoic tectonic evolution at middle of north margin of north China plate and provides a new basis for the study of crustal evolution of North China plate.
Keywords:Ondorsum group  oceanic crust reics  Neo-proterozoic era  north China plate  Baiyun′ebo
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