白云鄂博矿区H_9变质岩的Sm-Nd年龄、成因及与成矿关系
    点此下载全文
引用本文:张宗清,唐索寒,陈启桐,王进辉,袁忠信,白鸽.1997.白云鄂博矿区H_9变质岩的Sm-Nd年龄、成因及与成矿关系[J].地球学报,18(3):267-274.
DOI:
摘要点击次数: 2465
全文下载次数: 2269
作者单位
张宗清 中国地质科学院地质研究所 
唐索寒 中国地质科学院地质研究所 
陈启桐 中国地质科学院地质研究所 
王进辉 中国地质科学院地质研究所 
袁忠信 中国地质科学院矿床地质研究所 
白鸽 中国地质科学院矿床地质研究所 
中文摘要:本文报道了白云鄂博矿区H9变质岩富钾板岩,暗色板岩和变质基性火山岩的Sm-Nd年龄数据,讨论了上述变质岩的成因及与稀土矿床成矿关系。
中文关键词:Sm-Nd年龄  上伏变质岩  白云鄂博矿床
 
Sm Nd Ages and Origins of Metamorphic Rocks for the H 9 Formation in the Bayan Obo Ore District,and Relationship with the Ore Forming Event
Abstract:The Bayan Obo ore deposit in Inner Mongolia ,China is the largest REE deposit in the world.Many Words on this deposit have been made and vast amount of scientifil data have been accumulated.However,the origin ,especially ore_forming age have been ubder dispute for a long time. The geochronology of potassium_rich slates,dard slates and metabasic volcanitesfor the overling H 9 formation of the main ore body in the Bayan Obo ore deposit has been studied.Their Sm Nd ages have been obtained.The samples of the pottasium_rich slates present a Sm Nd isochron age of 1 096±56(2σ) Ma,with I Nd =0.51100±4(2σ),ε Nd (t) =-4.4±0.7.The Sm Nd isotopic analytical results of the 5 dark slate samples define a very good isochron of t =1 208±123(2σ) Ma with I Nd =0.51102±10(2σ),ε Nd ( t )=-1.1±1.9.The calculated isochron age of the 8 metabasic volcanic samples is 1 337±86(2σ) Ma,corresponding to I Nd =0.51091±6(2σ),ε Nd ( t )=-0.06±1.13. The Sm Nd isochron ages of the metamorphic rocks of the H 9 formation in the Bayan Obo ore district shows that the forming time for the ore deposit should be>1 000 Ma ,it implies ,the ore forming events chiefly took place in the middly Porterozoic. The Opinions that this ore deposit forms in the Calednian time of~400 Ma and the REE mineralization have two forming stages have not been demonstrated.The potassium rich slates,the dark slates and the metabasic volcanites have the variational ε Nd ( t ) values and ε Nd ( t )<0.But calculated ε Nd values are each other very close on condition of the same time and are in range of -0.4~-1.7 when t =1 286 Ma.It indicates that the metamorphic rocks of the H 9 formation in the Bayan Obo ore district, as this ore deposit which Sm Nd age of whole ore samples is 1 286±91(2σ) Ma ,with I Nd =0.51098±4(2σ),ε Nd ( t )=-0.06±0.78,have been derived from the mantle of LREE slight enrichment.
keywords:Sm Nd age  overling metamorphic rock  Bayan Obo ore deposit
查看全文  查看/发表评论  下载PDF阅读器
版权所有 《地球学报》编辑部 Copyright©2008 All Rights Reserved
主管单位:中华人民共和国自然资源部 主办单位:中国地质科学院
地址: 北京市西城区百万庄大街26号,中国地质科学院东楼317室 邮编:100037 电话:010-68327396 E-mail: diqiuxb@126.com
技术支持:北京勤云科技发展有限公司
京ICP备05029128号-6

京公网安备 11010202007616号