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

定向流体包裹体群的面状要素与微裂隙成生关系测量法
引用本文:韦昌山,翟裕生.定向流体包裹体群的面状要素与微裂隙成生关系测量法[J].地质科技情报,1996,15(3):81-85.
作者姓名:韦昌山  翟裕生
作者单位:中国地质大学
摘    要:阐述了定向流体包裹体群的面状要素与微裂隙关系测量方法(FIP法)的研究内容和研究步骤,并简述了该方法在构造、岩浆岩、矿床、沉积盆地油气田、地热等研究领域中的研究实例,指出该方法可适用于以含石英等成岩矿物为研究对象的研究领域,还可对传统的包裹体地球化学方法作出改进和提高。

关 键 词:FIP法  流体包裹体  古构造应力场--流体场  流体迁移  微裂隙  成岩矿物

FLUID INCLUSION PLANE METHOD---A METHOD FOR TIME/SPACE RECONSTRUCTION OF PALAEOSTRUCTURAL STRESS FIELD AND PALAEOFLUID MIGRATION FIELD
Wei Changshan,Zhai Yusheng.FLUID INCLUSION PLANE METHOD---A METHOD FOR TIME/SPACE RECONSTRUCTION OF PALAEOSTRUCTURAL STRESS FIELD AND PALAEOFLUID MIGRATION FIELD[J].Geological Science and Technology Information,1996,15(3):81-85.
Authors:Wei Changshan  Zhai Yusheng
Abstract:This paper presents a new method(FIP-fluid inclusion plane method)for quantitative time/space reconstruction on palaeostuctural stress field and palaeofluid migration field,and describes the research contents and the steps of this method.It is shown that the study of FIP has been applied successfully to many research fields of geoscience such as tectonics,magmatites,ore deposits,sedimentary basins and geothermal system etc.,in which quartz is investigated.
Keywords:FIP method  fluid inclusion groups  palaeostructural stress and palaeofluid migration fields  fluid movement  microfissures  
本文献已被 CNKI 维普 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