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安徽铜陵地区是我国长江中下游铜-铁-硫-金成矿带的重要组成部分,发育众多的铜、金、多金属矿床,同时燕山期岩浆岩广泛分布。区内金属矿床和岩浆岩一直是地质学家们关注和研究的热点。但是,到目前为止,研究者们对于该区岩浆岩的岩石系列、成因类型、成岩机制及成岩物质来源等观
The Tongling area in Anhui Province is an important part of the copper-iron-sulfur-gold metallogenic belt in the middle and lower reaches of the Yangtze River in China. There are many copper, gold and polymetallic deposits in the middle and lower reaches of the Yangtze River and the magmatic rocks in the Yanshan Period are widely distributed. The regional metal deposits and magmatic rocks have always been the focus of geologists’ attention and research. However, up to now, researchers have studied the rock series, genetic types, diagenetic mechanism and diagenetic source of magmatic rocks in this area