摘要
根据实测地温资料和岩石骨架热导率测试结果对本区今地温场的特征进行了分析，利用镜质体反射率反演古热流、成岩期原生矿物流体包裹体均一法测温和磷灰石裂变径迹的热史分析研究了本区的地热演化，所获得的认识对松辽盆地东南隆起区的油气地质研究和勘探评价很有意义。
The present-day geotempeature data of DST and thermoconductivity factor of rock skele ton with experiment were used to analyze the characteristies of the present-day geothermal field in the swell region of Southeast Songliao basin. Using paleoheat flux from analysis of inversion of vitrinite reflectance, homogenization temperatures from fluid inclusion thermometry in mineral of diagenetic stage and the geothermal history from apatite fission track analysis, the evolution of thermal history is determined for this area.The conclusions obtained from the research would be advantageous to the evaluation of the petroleum expolation and to the study of oil and gas geology in the swell area of Southeast Songliao basin.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1995年第3期328-334,共7页
Earth Science-Journal of China University of Geosciences
基金
"八五"国家重点科技攻关项目
关键词
地热史
液包体
古热流
古地温计
松辽盆地
geothermal history,vitrinite reflectance, fluid inclusion, apatite fission track,paleoheat flux,paleogeothermometer,Songliao basin.
