首页 | 本学科首页   官方微博 | 高级检索  
     检索      

西秦岭南亚带金-铜-铀成矿带中硅岩的海底喷流沉积特征研究
引用本文:郑明华,刘家军.西秦岭南亚带金-铜-铀成矿带中硅岩的海底喷流沉积特征研究[J].成都理工大学学报(自然科学版),1993(2).
作者姓名:郑明华  刘家军
作者单位:成都地质学院地质矿产勘查系 (郑明华),成都地质学院地质矿产勘查系(刘家军)
摘    要:经过野外与室内工作,作者首次提出,西秦岭南亚带Au-Cu-U成矿带中的硅岩乃海底喷流作用的产物。岩石学、岩石化学、微量元素、稀土元素、氧和硅同位素特征等为硅岩的海底喷流沉积成因提供了令人信服的证据。

关 键 词:金-铜-铀成矿带  硅岩  海底喷流沉积  西秦岭

ON THE SUBMARIN EXHALATIVE SEDIMENTATION NATURE OF SILICALITES FROM THE GOLD-COPPER-URANIUM METALLOGENIC BELT IN THE SOUTH SUBZONE OF WESTERN QINLING
Zheng Minghua Liu Jiajun.ON THE SUBMARIN EXHALATIVE SEDIMENTATION NATURE OF SILICALITES FROM THE GOLD-COPPER-URANIUM METALLOGENIC BELT IN THE SOUTH SUBZONE OF WESTERN QINLING[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1993(2).
Authors:Zheng Minghua Liu Jiajun
Institution:Zheng Minghua Liu Jiajun
Abstract:On the basis of field and laboratory studies, for the first time the authors propose that the silicalite which occured at the gold-copper-uranium metallogenic belt in the southern subzone of the western Qinling is a product of submarine exhalative sedimentation. The petrology and petrochemical characteristics of the trace element and rare earth element contents, silicon and oxygen isotopes, have provided convincing evidence to suggest the rock is of exhalative sedimentary origin.
Keywords:silicalite  gold-copper-uranium metallogenic belt  submarine exhalative sedimention  western Qinling
本文献已被 CNKI 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号