1) Liwu type copper deposit
里伍式铜矿
1.
It is pointed out that metallization of Liwu type copper deposits is controlled by magma-metamorphic core complexs,metallogenesis took place during middle to late stage of extension,and allocation of orebodies is controlled by fragile-ductile structures formed in middle to late stage.
本文通过矿床地质特征分析,结合区域地质成果,研究了里伍式铜矿矿化富集规律、找矿标志和找矿前景。
2) Liwu-typed Cu-riched deposits
里伍式富铜矿
3) Liwu copper deposit
里伍铜矿
1.
Quartz inclusions from the ore-bearing rocks in the Liwu copper deposit,Jiulong,Sichuan;
四川九龙县里伍铜矿包裹体研究
2.
Scanning electron microscopy and energy dispersive spectrum analysis of the ore minerals from the Liwu copper deposit,Jiulong,Sichuan
四川九龙里伍铜矿主要矿石矿物扫描电镜能谱分析
3.
The Liwu copper deposit is a typical medium-sized polymetallic deposit in the western margin of Yangtze terrane,which has a complex metallogenic setting and is potential for the prospecting.
里伍铜矿床位于扬子地台西缘,是中型铜多金属矿床,其成矿背景复杂,找矿潜力巨大。
5) Liwu Cu-Zn deposit
里伍铜锌矿床
1.
The Liwu Cu-Zn deposit is a typical medium-sized polymetallic deposit in the west of Sichuan province,which located in the west of Kangdian Earth s axis,the south edge of Songpan-Granze orogen and the northwest of Muli-Jinping arc thrust tectonic zone,and the deposit is the part of paleoproterozoic Cu-Zn polymetallic metallogenic belt of Jiulong-Muli metamorphic-thrust complex zone.
里伍铜锌矿床位于四川省西部,地处康滇地轴西侧,松潘—甘孜造山带东南缘,北东向木里—锦屏弧形推覆构造带北西侧,属九龙—木罩变质—推覆复合构造元古宙铜锌多金属成矿带,为川西典型的中型富铜锌多金属矿床。
6) Shijuli gold deposit
石居里铜矿
补充资料：乡伍
1.犹乡里。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条