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川东北地区长兴组-飞仙关组中金红石和菱锶矿的发现及成因解释
引用本文:刘欣,傅恒,李仲东,黄勇.川东北地区长兴组-飞仙关组中金红石和菱锶矿的发现及成因解释[J].成都理工大学学报(自然科学版),2011,38(3):321-327.
作者姓名:刘欣  傅恒  李仲东  黄勇
作者单位:1. 成都理工大学能源学院,成都,610059
2. 成都理工大学能源学院,成都610059;“油气藏地质与开发工程”国家重点实验室,成都610059
3. 中国石化勘探南方分公司研究院,成都,610021
摘    要:通过室内薄片研究,认为川东北地区长兴组-飞仙关组碳酸盐岩地层中赋存有自生金红石和菱锶矿.应用矿物学理论,并结合电子探针、扫描电镜和能谱成分等测试分析,结果表明金红石为中-晚成岩阶段形成的热水在运移过程中与富含绿泥石质泥土、黑云母碎片的碳酸盐岩围岩发生水岩反应,即从绿泥石、黑云母中析出的Ti元素结晶而成.菱锶矿为中-晓成...

关 键 词:川东北  金红石  菱锶矿  成因分析

Discovery and origin explanation of rutile and strontianite of Changxing-Feixianguan Formation in the northeast of Sichuan
LIU Xin,FU Heng,LI Zhong-dong,HUANG Yong.Discovery and origin explanation of rutile and strontianite of Changxing-Feixianguan Formation in the northeast of Sichuan[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2011,38(3):321-327.
Authors:LIU Xin  FU Heng  LI Zhong-dong  HUANG Yong
Institution:LIU Xin1,FU Heng1,2,LI Zhong-dong1,HUANG Yong11.College of Energy Resources,Chengdu University of Technology,Chengdu 610059,China,2.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,3.Institute of Southern Branch of SINOPEC,Chengdu 610041
Abstract:Based on the research of slices,the authors consider that there are authigenic rutile and strontianite in Changxing-Feixianguan Formation in the northeast area of Sichuan.The paper indicates that rutile and strontianite are generated respectively by the reactions between the geothermal hot water formed in middle-late diagenetic period and chlorite,carbonate rock in blackmica rich and between that and carbonate rock rich in strontium trough mineralogy theory and analyses including EMP,SEM,and energy spectrum...
Keywords:Northeast Sichuan  rutile  strontianite  mineral characteristics  origin analysis  
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