青海鄂莫切德地区水系沉积物异常以Pb、Zn、Cd元素为主,异常浓度分带清晰,峰值极高,且异常套合紧密,表现为中低温成矿元素组合特征。发现的Pb Zn Cu矿化呈细脉状、斑点状、薄膜状赋存于岩石裂隙或表面,褐铁矿化强烈,岩石内部元素含量并不高,热液作用迹象明显。 Pb, Zn and Cd were the main anomalies in the sediments of the E Moqide area in Qinghai Province. The anomalous concentration bands were clear, the peaks were extremely high, and the anomalies were closely interbedded. The characteristics of the mineral assemblages were characterized by medium and low temperature. Pb Zn Cu mineralization was found in veinlets, spots, thin film occurs in the rock fissures or surface, strong iron mineralization, the rock element content is not high, obvious signs of hydrothermal.