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铜陵新桥胶状黄铁矿纳米矿物学特征及成矿意义
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摘要
<正>长江中下游成矿带是中国东部重要的铜(金、铁)多金属成矿带,矿带内发育层状铜(金)多金属硫化物矿床,铜陵地区为成矿带内典型层状铜(金)多金属硫化物矿集区。矿区内层状铜(金、铁)硫化物矿床受控于中-上石炭统、上二叠统和中-下三叠统碳酸盐地层,但是层状铜多金属硫化物矿体主要产于中-上石炭统黄龙组和船山组。学者们对铜陵地区铜(金)多金属硫化物矿体成因进行了大量研
引文
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