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1)  Machangqing Cu-Mo-Au deposit
马厂箐铜钼金矿床
2)  Machangqing Cu-Mo deposit
马厂箐铜钼矿床
1.
The early metallogenesis of the Machangqing Cu-Mo deposit occurred at about 37-40 Ma, while the late metallogenesis occurred at about 34-35 Ma, just in consis.
马厂箐铜钼矿床早期成矿发生在37~40Ma左右,晚期成矿大约在34~35Ma;与区域上其它与富碱侵入岩有关矿床的形成时间相当吻合。
3)  Cu-Mo polymetallic deposit
铜钼多金属矿床
4)  Mo-Cu polymetallic deposit
钼铜多金属矿床
1.
The Bangpu Mo-Cu polymetallic deposit is one of the typical large-scaled porphyry deposit,lies in eastern Gangdese metallogenic belt,Tibet.
邦铺钼铜多金属矿床位于西藏冈底斯斑岩铜矿带东段,是典型的大型斑岩型钼铜矿床。
5)  copper-molybdenum deposit
铜钼矿床
1.
A discussion on the alteration features of the copper-molybdenum deposit in Wunugetu Mountain,Mongolia;
内蒙古乌奴格吐山铜钼矿床围岩蚀变特征浅析
6)  Cu-Mo deposit
铜钼矿床
1.
Geological features of Yantang Cu-Mo deposit in eastern Hainan Island;
海南琼海烟塘梅岭铜钼矿床地质特征
2.
By the study on the geological and geochemical characteristics of the Cu-Mo deposit in Huangbaiyu area,it's ore-forming condition is discussed.
通过阐述黄柏峪铜钼矿床的地质特征及地球化学特征,来探讨其成矿地质条件,认为该区不仅存在矽卡岩型矿床,而且也有斑岩型及热液型矿床存在的可能。
补充资料:马厂
1.牧马场。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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