摘要
随着地质调查的逐渐深入,发现在旱平川断陷盆地东南部有地热异常显示。经进一步勘探,在孔深1200m时,井温已达40oC以上,盆地南、北两条断层(Fl、F2)为该区地热田的控热构造,第三系杨梢组为旱平川断陷盆地的地下热水储层,其补给条件好、地下热水资源丰富,具有良好的开发前景。
Along with deepgoing of geologica l research gradually,the geothermal abnorm ality in south-eastern basin was discovere d.Through further exploration found that w ell temperature in depth 1200m reached more than 40℃,the 2 faults (F,F)located south a nd north of basin are heat-controlled struc ture of geothermal field in the area,and Ya ngshao formation of Tertiary system is rese rvoir of ground hot water in Hanpingchuan g raben-faulting basin,and there are better recharge condition and abundant ground hot water resources,so it has possessed good pr ospect of exploitation.
出处
《中国煤田地质》
2002年第4期42-43,54,共3页
Coal Geology of China
