1) Dahenglu cobalt deposit
大横路钴矿床
2) Dahenglu Co Cu deposit
大横路钴铜矿床
1.
Dahenglu Co Cu deposit is located in the middle section of Liaoning and Jilin Early Protorozoic rift, south flank of Laoling anticline, lithologically, the host rock for this deposit is the middle section of Dalizi Formation, Laoling Group, which consists of a suite of lightly metamorphosed rock series.
吉林省大横路钴铜矿床赋存于辽吉早元古宙裂谷中段、老岭背斜的南翼，具体层位为老岭群大栗子组的中部岩性段，属于一套浅变质岩系。
3) Dahenglu CuCo deposit
大横路Cu-Co矿床
4) cobalt deposit
钴矿床
1.
The fluid inclusions of Tuolugou cobalt deposit are studied by Homogenization Method and Laser Raman Method.
应用均一法、激光拉曼显微探针法研究驼路沟钴矿床的流体包裹体,发现其包裹体类型多样,以气液两相包裹体和富二氧化碳包裹体为主,测得均一温度为220℃~300℃,众值为275℃,成矿流体形成于中低温环境。
2.
This paper is based on cobalt mineral resources in the world today, classification of cobalt deposits and the latest advances of exploration and research on cobalt deposits home and abroad.
本文概述了当前世界钴资源状况、钴矿床分类及国内外钴矿床勘查与研究的最新进展。
3.
The Wubaoshan deposit is a new type cobalt deposit found in Jiangxi.
五宝山钴矿床是江西省新类型钴矿床。
5) Cu & Co deposit
铜-钴矿床
1.
Haerhan (Dulenggou) Cu & Co deposit is located in the east of Dongkunlun polymetalic mineralization zone.
哈尔汗(督冷沟)铜-钴矿床位于东昆仑多金属成矿带东段。
6) Cu-Co deposit
铜钴矿床
1.
The Dulengou Cu-Co deposit is located in the eastern area of Kunlun metallogenic belt.
督冷沟铜钴矿床位于近EW向东昆仑构造带东段,它形成于晚古生代岛弧环境,成矿地质作用非常复杂,绿泥绢云母千枚岩为主要赋矿地层,构造变形使矿质运移、富集。
补充资料：大横
大横
足太阴脾经穴。在腹中部，距脐中4寸。
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