贵德盆地热结构及地热成因机制
发布时间：2018-08-19 08:55
【摘要】：正贵德盆地位于青藏高原东北缘黄河谷地之中,四周环山,为新生代断陷盆地,地貌单元位于青藏块体,地处祁连、昆仑和秦岭三大褶皱系交汇地带;新构造活动强烈,发育一系列NWW向、NW向及NNW向断裂,为区内高温地热系统提供了较好的地热地质条件。区内地热显示类型多样,水热活动剧烈,尤其是盆地西部的扎仓寺热田,水温高达93℃,蕴藏着丰富的地热资源。但是由于客观条件
[Abstract]:The ZhengGuide basin is located in the Yellow River valley in the northeast margin of the Qinghai-Tibet Plateau, surrounded by mountains, is a Cenozoic faulted basin, and the geomorphologic unit is located in the Qinghai-Tibet block, which is located at the intersection of the three major fold systems of Qilian, Kunlun and Qinling. A series of NWW trending NW faults and NNW trending faults have been developed, which provide a good geothermic geological condition for the high temperature geothermal system in the region. There are various types of geothermal in the area, especially the Zacang Si hot field in the western part of the basin. The water temperature is as high as 93 鈩，
本文编号：2191170
[Abstract]:The ZhengGuide basin is located in the Yellow River valley in the northeast margin of the Qinghai-Tibet Plateau, surrounded by mountains, is a Cenozoic faulted basin, and the geomorphologic unit is located in the Qinghai-Tibet block, which is located at the intersection of the three major fold systems of Qilian, Kunlun and Qinling. A series of NWW trending NW faults and NNW trending faults have been developed, which provide a good geothermic geological condition for the high temperature geothermal system in the region. There are various types of geothermal in the area, especially the Zacang Si hot field in the western part of the basin. The water temperature is as high as 93 鈩，
本文编号：2191170
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