摘要
Many geologists have been interested in the colourful geology of the Karamaili area, located in the south of east Junggar, Xinjiang. Ren et al. suggested that the Karamaili fault belt which is in NWW-trending might be one of the latest sutures of the paleo-Junggar ocean and that basic and ultrabasic rocks exposed
基金
Project supported by the National 305 Project of China and the National Natural Science Foundation of China