CAJ | 학술논문

山东省的深部岩溶热储分布在济阳坳陷区、临清坳陷区的凸起（潜）区和鲁中隆起区、鲁西南潜隆起区、沂沭断裂带，分布面积约4．4万 km2，其分布范围与寒武-奥陶纪地层分布基本一致。深部岩溶热储可划分深部裂隙-岩溶热储和深部岩-溶裂隙热储2种类型，具层状及层状兼带状特征。该文在总结前人成果的基础上，对深部岩溶热储的埋藏与分布、水质、地温场特征、深部岩溶发育规律和地热流体形成条件进行了论述，以期能对开发利用这一热储有所帮助。
산동성적심부암용열저분포재제양요함구、림청요함구적철기（잠）구화로중륭기구、로서남잠륭기구、기술단렬대，분포면적약4．4만 km2，기분포범위여한무-오도기지층분포기본일치。심부암용열저가화분심부렬극-암용열저화심부암-용렬극열저2충류형，구층상급층상겸대상특정。해문재총결전인성과적기출상，대심부암용열저적매장여분포、수질、지온장특정、심부암용발육규률화지열류체형성조건진행료논술，이기능대개발이용저일열저유소방조。
Deep karst thermal reserves distribute in Jiyang depression area ,convex(latern)area of Linqing de-pression and Luzhong uplift area ,southwestern latern uplift area in Shandong province and Yishu fault belt .Its distribution square is about 44000km2 ,and the distribution ranges are the same with the strata in Cambrian Ordovician period .Deep karst reserves can be divide into deep crack karst reserve and deep karst crack reserve with the characters of layer type and strip type .On the basis of previous research re-sults and the ideas of the authors ,burying ,distribution ,water quality ,characteristics of geothermosite , developing law of deep karst and the forming condition of geothermal fluid have been analyzed .It will pro-vide help for development and utilization of thermal reserve .