摘要
南迳地区位于赣南地区,区域上处于南岭东西向复杂构造带东段边缘与武夷山新华夏系隆起带西缘交接复合影响部位,地属雩山隆起带,构造运动强烈,岩浆活动频繁。通过开展可行性勘查工作,本区发现了优质资源。南迳地区可行性勘查工作中采用了多种地球物理勘探方法,通过相互对比和验证,基本查明了断裂构造的空间分布、性质、控导热性能、富水性等条件,为下一步开展钻探施工工作提供了重要依据。
The Nanjing geothermal area is located in the southern part of Jiangxi Province,which is located at the junction of the eastern margin of the Nanling east-west complex tectonic belt and the western margin of the Wuyishan Xinhuaxia uplift belt.The area belongs to the Yushan uplift belt,with strong tectonic movement and frequent magmatic activity.High quality geothermal water resources have been found in this area by carrying out feasibility survey.Several geophysical exploration methods have been adopted in the feasibility exploration of Nanjing geothermal area,and the spatial distribution,properties,controlling thermal conductivity and water-rich conditions of the fault structures have been basically ascertained through mutual comparison and verification,which provides an important basis for further drilling and construction.
作者
徐良
杨倩
XU Liang;YANG Qian(Hydrogeology Engineering Geology Brigade,Jiangxi Bureau of Geology and Mineral Exploration and Development,Nanchang 330000,China)
出处
《世界有色金属》
2019年第19期176-177,共2页
World Nonferrous Metals
关键词
南迳地区
多种地球物理勘探方法
断裂构造
nanjing area
several geophysical exploration methods
fracture structure
