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青海共和盆地地热资源分布特征兼述CSAMT在地热勘查中的作用
引用本文:王斌,何世豪,李百祥,宋窑东.青海共和盆地地热资源分布特征兼述CSAMT在地热勘查中的作用[J].矿产与地质,2010,24(3):280-285.
作者姓名:王斌  何世豪  李百祥  宋窑东
作者单位:1. 青海省第二水文地质工程地质勘察院,西宁,810008
2. 甘肃省地矿局第二地勘院,兰州,730020
3. 重庆地质仪器厂,重庆,400033
摘    要:青海共和盆地为一新生代断陷盆,具有良好地热地质背景与其东、西两侧构造岩浆带断裂型地热分布,构成秦昆接合部SN向地热带。另据CSAMT在海南州首府共和县恰卜恰镇地热勘查推断出一小型拉分盆地,兼有盆地传导型层状热储和断裂对流型带状热储的特征,提出拟建地热井位钻孔布置构造有利部位,建议孔深1200m。经钻探打出全省第一口水温高、水量大、水质优的地热井,发挥了CSAMT在地热勘查中的指导作用。

关 键 词:地热资源  可控源音频大地电磁测深(CSAMT)  地热勘查  共和盆地

Geothermal resource distribution characteristics of Gonghe basin in Qinghai——Effect of CSAMT in geothermal prospecting
WANG Bin,HE Shi-hao,LI Bai-xiang,SONG Yao-Dong.Geothermal resource distribution characteristics of Gonghe basin in Qinghai——Effect of CSAMT in geothermal prospecting[J].Mineral Resources and Geology,2010,24(3):280-285.
Authors:WANG Bin  HE Shi-hao  LI Bai-xiang  SONG Yao-Dong
Institution:1.Second Qinghai Hydrology & Geo-engineering Institute,Xining 810008;2.Second Institute of Geological and Mineral Exploration of Gansu Provincial Bureau of Geology and Mineral Resources,Lanzhou 730020;3.Chongqing Geological Instrument Factory,Chongqing 400033)
Abstract:Gonghe basin in Qinghai is a Cenozoic depression basin with good geothermal geological background and geothermal distribution of fracture type on both east and west sides of fracture-magmata belt,forming a S-N striking geothermal belt.In addition,based on CSAMT survey,a small scale pull-apart basin has been extracted,showing the characteristics of basin conducted layer-shaped thermal reservoir and fracture convection type zonal thermal reservoir.A favorable location for the planned geothermal well drilling site is proposed in the paper,with a suggested hole depth of 1200m.A geothermal well with higher temperature, large water volume and superior water quality was hit by drilling and it shows that CSAMT is of great significance in guiding geothermal prospecting.
Keywords:geothermal resource  CSAMT  geothermal prospecting  Gonghe basin  Qinghai
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