【摘要】：正貴德盆地位于青藏高原東北緣黃河谷地之中,四周環(huán)山,為新生代斷陷盆地,地貌單元位于青藏塊體,地處祁連、昆侖和秦嶺三大褶皺系交匯地帶;新構(gòu)造活動強(qiáng)烈,發(fā)育一系列NWW向、NW向及NNW向斷裂,為區(qū)內(nèi)高溫地?zé)嵯到y(tǒng)提供了較好的地?zé)岬刭|(zhì)條件。區(qū)內(nèi)地?zé)犸@示類型多樣,水熱活動劇烈,尤其是盆地西部的扎倉寺熱田,水溫高達(dá)93℃,蘊(yùn)藏著豐富的地?zé)豳Y源。但是由于客觀條件
[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，

本文編號：2191170