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 diagenesis of Eocene Carhonate rocks in Kashi Depression. The Characteristics of fluid inclusion in diagenetic minerals are studied.According to the micro-measuring temperture and the studying on re-equilibrium of the inclusions, the diagenetic-geo-tempreture and the largest paleo-geotemperture have been obtained. Based on the above researsh, the oil-generating strata in this area are evoluated.
关键词
油气藏
地质构造
液包体
油气评价
喀什凹陷
Diagenesis,Fluid inclusion,Re-equilibrium of inclusion,Paleo-geotempreture,Oil-gas evoluation,Kashi depression
