滇西北雪鸡坪斑岩型铜矿构造特征与成矿作用研究
Structural Characteristics and Mineralization of Xuejiping Porphyry Copper Deposit in Northwest Yunnan
(a)岩石节理裂隙较为发育，并发育有大量的黄铁矿（Py）±黄铜矿（Ccp）+石英脉（Q）体充填；(b)呈浸染状分布的黄铜矿；(c)黄铜矿呈浸染状分布在微裂隙中，黄铁矿发育有压碎结构
滇西北雪鸡坪斑岩型铜矿构造特征与成矿作用研究 |
| 刘学龙,杨富成,张昌振,罗应,王帅帅 |
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Structural Characteristics and Mineralization of Xuejiping Porphyry Copper Deposit in Northwest Yunnan |
| Xuelong LIU,Fucheng YANG,Changzhen ZHANG,Ying LUO,Shuaishuai WANG |
| 图3 雪鸡坪铜矿区矿化显微特征 (a)岩石节理裂隙较为发育，并发育有大量的黄铁矿（Py）±黄铜矿（Ccp）+石英脉（Q）体充填；(b)呈浸染状分布的黄铜矿；(c)黄铜矿呈浸染状分布在微裂隙中，黄铁矿发育有压碎结构 |
| Fig.3 Microscopic characteristics of mineralization in Xuejiping copper ore district |
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