煤田地质与勘探2024，Vol.52Issue(1)：26-35,10.DOI:10.12363/issn.1001-1986.23.11.0721
松辽盆地岩石热导率柱及古地温场分布特征
Thermal conductivity column of rocks and distribution characteristics of paleo-geothermal field in the Songliao Basin
摘要
Abstract
The paleo-geothermal field of a basin is closely related to the formation and evolution of geothermal,oil,and gas resources.To ascertain the characteristics of the paleo-geothermal field in the Songliao Basin during some critical periods,this study established the thermal conductivity column of rocks in the basin using measurements from 269 samples and compiled previous data.Then,it simulated the burial and thermal histories of multiple wells under the con-straint of vitrinite reflectance(Rran).The results indicate that the thermal conductivity of the Songliao Basin increases with the depth,with increasing rates higher in the upper strata than in the lower strata and an average of 1.79 W/(m·K).Furthermore,the thermal conductivity also increases with the age of strata.The Rran of the northern Songliao Basin primarily ranges from 0.8% to 1.6% ,peaking in the Qijiagulong sag.The burial and thermal histories reveal that the pa-leo-geotemperature of the Cretaceous Qingshankou Formation peaked in the late stage of the Mingshui Formation depos-ition,followed by a gradual decrease until the present.The planar distribution of the paleo-geothermal field indicates that the Qingshankou Formation in the northern Songliao Basin exhibited a maximum paleo-geotemperature of above 120℃ in most areas,which is significantly higher than the present level.The basin entered the thermal subsidence stage after the deposition of the Qingshankou Formation,and its paleo-geotemperature gradually peaked with an increase in the pa-leo-burial depth.In this stage,the high paleo-geotemperature was favorable for the maturation of shale oil and gas.In the late stage of the Mingshui Formation,the Songliao Basin underwent a notable uplifting and cooling event under the in-fluence of the movement of the Paleo-Pacific Plate.In the cooling process,areas with a small decreasing amplitude of the geothermal gradient became favorable areas of geothermal conditions.The results of this study will provide a theor-etical reference for research on the formation mechanisms of geothermal,oil,and gas resources in the Songliao Basin.关键词
松辽盆地/古地温场/热导率/镜质体反射率/埋藏史-热史Key words
Songliao Basin/paleo-geothermal field/thermal conductivity/vitrinite reflectance/burial-thermal histories分类
天文与地球科学引用本文复制引用
唐博宁,邱楠生,朱传庆,常健,李潇,黄越,杨俊生,付秀丽..松辽盆地岩石热导率柱及古地温场分布特征[J].煤田地质与勘探,2024,52(1):26-35,10.基金项目
国家重点研发计划项目(2021YFA0716003) （2021YFA0716003）
