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松辽盆地地热资源的形成与远景评价
引用本文:谭世燕,石义强,赵育捷. 松辽盆地地热资源的形成与远景评价[J]. 世界地质, 2001, 20(2): 155-160,2091
作者姓名:谭世燕  石义强  赵育捷
作者单位:黑龙江省水文地质工程地质勘察院,
摘    要:松辽平原在地貌和地质上都是一个盆地。盆地中心区域上地幔隆升形成地幔枕,使本地区成为地壳中的一个热点,具有较高的地热背景。盆地是汇水区,盆地中部地域自然就成为地下热水主要的分布区。松辽盆地地热资源开发远景大有希望。

关 键 词:地台型裂谷盆地 中低温热水田 中低温传导-对流复合型地热系统 地热资源 开发远景 松辽盆地
文章编号:1004-5589(2001)02-0155-06

The Formation and Prospective Evaluation of Geothermal Resources in The Songliao Basin
TAN Shi_yan,SHI Yi_qiang,ZHAO Yu_jie. The Formation and Prospective Evaluation of Geothermal Resources in The Songliao Basin[J]. Global Geology, 2001, 20(2): 155-160,2091
Authors:TAN Shi_yan  SHI Yi_qiang  ZHAO Yu_jie
Abstract:The Songliao plain is a basin in both topography and geology. As a result of the upper mantle upwelling area of the centre part of the basin forming the mantle pilliow, the region became a heat point in the crust with the high geothermal setting. The basin is a collection area, of which the middle part became the developing area of geothermal water. The prospective exploition of geothermal resources be full of promise in the Songliao basin.
Keywords:geoheat  basin of rift valley of platform type  hot water field in the middle and low temperature  geothermal systems of conductive-conevctive heat flow integrative type in the middle and low temperatures.
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