论文部分内容阅读
南祁连山主脊青海省境内柴达木山—大哈尔腾河一带,属高寒山区,海拔高程一般均在4,000～5,000米之间,最高5,742米(柴达木山)。4,000米以上多现代冰川。该区地质研究程度很低,基本上属于地质空白区,仅在五十年代由中国科学院祁连山地质队进行过路线地质调查。1982年甘肃区域地质调查队二分队在这一带进行科学地质考察时,获得了较多的地质资料。现将地层方面的主要成果报导如下:
The main ridge of the South Qilian Mountains Qinghai Province Qaidam - Dawar Teng River area, is an alpine mountain, elevation are generally 4,000 ~ 5,000 meters above sea level, the highest 5,742 meters (Qaidam Mountains). More than 4,000 meters of modern glaciers. Geological research in this area is very low, basically belongs to the geological blank area, only in the fifties by the Chinese Academy of Sciences Qilian Mountains geological team conducted route geological survey. 1982 Gansu regional geological survey team second detachment in this area for scientific geological inspection, access to more geological data. The main achievements of the strata are reported as follows: