喀什凹陷第三纪灰岩流体包裹体及其应用研究  

FLUID INCLUSION STUDY OF EOCENE CARBONATE ROCKS IN KASHI DEPRESSION

作　　者：李昌存[1] 韩秀丽[1] 

机构地区：[1]河北理工学院,唐山063009

出　　处：《矿物学报》1998年第1期46-51,共6页Acta Mineralogica Sinica

摘　　要：本文在成岩作用研究的基础上，对喀什凹陷第三纪灰岩中的流体包裹体作了初步研究。通过包裹体的显微测温及包裹体的再平衡研究，得出了该区灰岩的成岩温度及其经历的最大古地温，并利用包裹体资料对该区的生油岩作了初步评价。This paper deals with the diagenes of Eocene carbonate rocks in the Kashi Depression.The fluid inclusion characteristics of diagenetic minerals are described. In term of the micro-ther-mometry and reequilibrium data on the fluid inclusions,the diagenetic temperature and maximumpale0-geotemperature have been obtained' Based on the above data,the oil-generating strata in thisarea are evaluated.

关 键 词：成岩作用 喀什凹陷 液包体 灰岩 第三纪 

分 类 号：P588.245[天文地球—岩石学]