1) porphyry copper
斑岩铜（金）矿床
2) porphyry copper-gold deposit
斑岩铜-金矿床
3) Shaxi-Changpushan por-phyry Cu-Au deposit
沙溪-菖蒲山斑岩铜金矿床
4) porphyry
斑岩
1.
The geological features and genetic pattern of Te-Au deposit related to porphyry in North Qilian Mts;
北祁连山与斑岩有关的碲金型金矿床地质特征和成因模型
2.
Geochemistry of the Eocene-ligocene porphyry in the Narigongma region,Qinghai;
青海纳日贡玛始新世—渐新世含矿斑岩体地球化学特征
3.
The orebodies of the Gongpoquan copper orefield occur in the quartz dioritic porphyry body, granodioritic porphyrite body and dacitc porphyry body.
公婆泉铜矿矿体的赋矿围岩主要为石英闪长玢岩、花岗闪长斑岩和英安斑岩 ,这些含铜斑岩体形成于晚志留 -早泥盆世板块俯冲碰撞过程中 ,受断裂和火山机构控制。
5) porphyries
斑岩
1.
The early magmatic rocks include quartz syenite porphyries, syenite porphyries, striking in near SN direction; the latter ones include biotite syenite porphyries, lamprophyres, striking in near EW direction.
详细讨论了北衙矿区的地质特征,通过对勘探资料的深入研究和野外观察,初步确定,北衙矿区存在两期岩浆活动,早期的石英正长斑岩、正长斑岩等近南北向分布,晚期的黑云正长斑岩、煌斑岩脉等呈近东西向展布。
2.
Based on detailed geological observation and precise dating of porphyries in combination with data available, the authors hold that the Indosinian porphyries in the Zhongdian island arc zone can be divided into two parts, i.
在较为详细的野外地质观测和精确的同位素测年的基础上 ,结合前人资料 ,将中甸地区的印支期岛弧斑岩体分为东、西两个斑岩带 ,东斑岩带形成于 2 1 8～ 2 0 3Ma ;西斑岩带形成于 2 4 2 。
6) Western Porphyry
西部斑岩
1.
Relationship between Western Porphyry and mineralization in Qulong copper deposit of Tibet and its enlightenment to further exploration;
西藏驱龙铜矿西部斑岩与成矿关系的厘定:对矿床未来勘探方向的重要启示
参考词条
补充资料：铜金
1.即铜。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。