摘要
采用水文地球化学方法,根据青岛地区50多个地下水样品的测试分析结果进行了地下热储温度的推测,结合遥感解译、测温、地质背景条件等资料综合分析,圈定出3个地热远景区,即温泉地热远景区、黄家山地热远景区和流亭地热远景区,这3个地热远景区均分布在NNE向断裂与NW向断裂交汇部位上。通过对该区地热地质特征初步分析认为,其热储概念模型属深循环对流型。
Using geohydrochemical method, and according to determ ination and analysis results of more than 50 underground water samples in Qingda o area, underground heat reserve temperature is inferred. Combining with remote sense interpretation, thermometry and geological background condition to analyse complicately, 3 geothermal future areas are circled as hot spring geothermal fu ture area, Huangjiashan geothermal future area and Liuting geothermal future are a. These three geothermal future areas all distribute in contacting section of N NE fault and NW fault. Through primary analysis of geological characteristics of geotherm in Qingdao area, it is regarded that heat reserve model belongs to dee p-circulation convective type.
出处
《山东地质》
2003年第2期46-49,56,共5页
Geology of Shandong
关键词
水化学方法
青岛市
地热资源
地热地质特征
地下热储温度
Geothermal future area
geohydrochemistry
geologic al characteristics of geotherm
Qingdao city
