摘要
白牡岭地区位于长江中下游成矿带铜陵矿集区的北部。本文对安徽省铜陵白牡岭地区铅锌有色金属矿床的地质特征进行了详细的介绍;并探讨了该矿床的成因,认为其成因和地下热液作用有关,提出为沉积+热液叠改型的认识。
White Hart Ridge area is located in the Yangtze River metallogenic belt north of Tongling Ore District. In this paper, the geological characteristics of Tongling Nonferrous Metals White Hart Ridge area of lead and zinc deposits were introduced in detail; and discusses the genesis of the deposit, that its causes and effects related to underground hydrothermal proposed modifications stacked sedimentary hydrothermal + understanding.
出处
《世界有色金属》
2016年第13期206-208,共3页
World Nonferrous Metals
关键词
安徽省铜陵
白牡岭地区
铅锌有色金属矿床
地质特征
矿床成因
Geological Characteristics
Tongling
white male Ridge area
non-ferrous metals lead and zinc deposit
deposit
