论文部分内容阅读
在爱达荷钴带的南东端,穿过若干矿化带,在九处采集了河流沉积物和水成苔藓样品。由于该地区地势徒峻、水流湍急,很难采到合适的沉积物样
At the southern end of the Idaho Cobb, several mineralized zones were traced and river sediments and water-moss samples were collected at nine sites. Due to the steep terrain and rapid current in the area, it is difficult to obtain suitable sediment samples