贵州区域地热成因探讨

王亮, 胡从亮, 张嘉玮, 陈国勇, 张美雪, 杨武, 张应文

Exploration of the genesis of regional geothermal resources in Guizhou Province

WANG Liang, HU Cong-Liang, ZHANG Jia-Wei, CHEN Guo-Yong, ZHANG Mei-Xue, YANG Wu, ZHANG Ying-Wen

图1 贵州地热资源分布[9] 1—裂隙型带状层状复合型热储层分区;2—裂隙型带状热储层分区;3—岩溶型层状热储层分区;4—尚待查明区;5—主要断裂;6—25~40℃温泉;7—40~60℃温泉;8—60~90℃温泉;9—25~40℃地热井;10—40~60℃地热井;11—60~90℃地热井;12—90~150℃地热井

Fig.1 Distribution of geothermal resources in Guizhou[9] 1—layered fractures compound geothermal reservoir;2—banded fractures geothermal reservoir;3—layered karst thermal reservoir;4—others to be determined;5—major faults;6—hot spring at 25~40℃;7—hot spring at 40~60℃;8—hot spring at 60~90℃;9—geothermal well at 25~40℃;10—geothermal well at 40~60℃;11—geothermal well at 60~90℃;12—geothermal well at 90~150℃