CAJ | 학술논문

通过对地质资料的分析，认为该区理论上具有较好的地热生成环境和赋存条件。重点围绕！？葛沟断裂两侧，综合运用地质调查、测温、物探、钻探等手段，对成热地质条件进行调查分析，圈定淳于地热异常区和梁家庄地热异常区2个异常区，分析并初步确定热源为地壳深部的热流，导水导热通道为！？葛沟断裂及其次级断裂，热储为深循环对流型带状热储，热储岩性为白垩纪青山群安山岩，埋深1400～2000 m，盖层为新近纪、古近纪及白垩纪粘土岩、砂岩等。结合区域地质资料，建立地热资源概念模型，并据此确定了3处拟井位置及孔深。
통과대지질자료적분석，인위해구이론상구유교호적지열생성배경화부존조건。중점위요！？갈구단렬량측，종합운용지질조사、측온、물탐、찬탐등수단，대성열지질조건진행조사분석，권정순우지열이상구화량가장지열이상구2개이상구，분석병초보학정열원위지각심부적열류，도수도열통도위！？갈구단렬급기차급단렬，열저위심순배대류형대상열저，열저암성위백성기청산군안산암，매심1400～2000 m，개층위신근기、고근기급백성기점토암、사암등。결합구역지질자료，건입지열자원개념모형，병거차학정료3처의정위치급공심。
Through analysis on geological data,it is regarded that there are good forming environment and occur-rence conditions of geothermal in this area.Focusing on both sides of Tangwu-Gegou fault belt,by using geolog-ical survey,temperature measurement,geophysical exploration,drilling and other means,geological conditions of geothermal have been surveyed and analyzed.Chunyu geothermal and Liangjiazhuang geothermal anomaly zone have been circled.After analysis,it is determined that the heat source is initially deep crustal heat flow,and ther-mal conductivity water channels are Tangwu-Gegou fault and its secondary faults.Thermal reservoir is deep con-vection and ribbon type.lithology of geothermal reservoir is andesite in Cretaceous Qingshan group with the depth of 1400~2000m.Its covering layers are Neogene,Paleogene and Cretaceous claystones and sandstones.Combi-ning with regional geological data,a conceptual model of geothermal resources has been set up,and location and hole depth of three proposed wells have been accordingly determined.