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一、前言阿木尼克山,位于青海省柴达木盆地之东北缘(图1)。前人对该区出露的石炭系曾做过初步研究,划有中下石炭统或下石炭统。1975年青海区调一队四分队在开展1:20万托素湖幅区调期间,于同年9月在中国地质科学院部分同志的协助下测制了该区石炭系剖面,经初步研究认为该区有早石炭世杜内期的沉积。1977年6月至7月,区调一队综合分队与四分队乔金良、洪哲生,中国地质科学院詹立培、王增吉、王士涛、严克明等同志共
I. Foreword Amunick Hill, located in the northeastern margin of the Qaidam Basin in Qinghai Province (Figure 1). The predecessors did a preliminary study on the Carboniferous exposed in the area, with the Middle-Lower Carboniferous or Lower Carboniferous. In 1975, a unit of the first team in Qinghai District, during the 1: 200,000-ton-Ton Lake range adjustment, measured the Carboniferous section of the area with the assistance of some comrades of the Chinese Academy of Geological Sciences in September of the same year. After preliminary study, The area has early Carboniferous Dunes deposition. From June to July 1977, a team of integrated units and Qiaoshou Qiao Jinliang, Hong Zhensheng, the Chinese Academy of Geological Sciences Zhan Lipei, Wang Zengji, Wang Shitao, Yan Keming and other comrades