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作 者:张俊宝
机构地区:[1]东北煤田地质局一○七勘探队,辽宁阜新123000
出 处:《中国煤田地质》2003年第6期37-39,共3页Coal Geology of China
摘 要:根据东梁区DR-1与DR-2地热井及以往地质资料,对控制本区地热资源的赋存条件(热储层、控热构造及盖层)作了研究后认为,该区的地热资源主要受控于热储构造、热储层裂隙的发育程度和盖层条件,而热储层裂隙的发育程度及与含水层的水力联系,又决定了本区地下热水的开发潜能。According to DR-1,DR-2geoth er mal wells and formerly obtained geological information,and after analyzed the h osting condition(geothermal reservoir,geothermal controlling structures and co ver strata)that controlling the geothermal re-sources this district,the autho r considered:geothermal resources in the district is mainly controlled by geoth ermal reservoir structures,fracturing degree of reservoir and cover strata cond itions,while the fracturing degree and its hydraulic connection with aquifers i s determining exploitation potential of geothermal water this district in turn.
分 类 号:P314.2[天文地球—固体地球物理学]
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