1) Gangdese copper belt
冈底斯铜矿带
1.
Petrological,geochemical and Nd,Sr,Pb isotopic studies indicate that the ore-hosting volcanic rocks of Xiongcun supperlarge copper-gold deposit in the Gangdese copper belt, Tibet belong to dacite porphyry with ultro-shallow emplacement.
岩石学、地球化学和Nd、Sr、Pb同位素研究表明,西藏冈底斯铜矿带雄村特大型铜金矿床的容矿火山岩为一套具超浅成侵入特点的英安斑岩,SiO2含量集中在61。
2) Gangdise copper belt
冈底斯铜带
3) Gangdese porphyry copper belt
冈底斯斑岩铜矿带
1.
New zircon U-Pb ages of the Chongjiang and the Qulong ore-bearing porphyries in the Gangdese porphyry copper belt are analyzed by using ELA-ICP-MS dating technique.
利用ELA-ICP-MS分析技术对冈底斯斑岩铜矿带冲江及驱龙含矿斑岩体进行锆石U-Pb年龄测定,所得到的年龄分别为14。
2.
The Gangdese porphyry copper belt is a new discovered ore belt in South Tib et,China.
青藏高原南部冈底斯斑岩铜矿带冲江含矿斑岩早期为闪长岩,主期为花岗闪长斑岩及石英二长斑岩,晚期为花岗斑岩。
3.
The Gangdese porphyry copper belt is a new discovered ore belt in the South Tibet, China.
冈底斯斑岩铜矿带是在藏南新发现的铜矿带。
5) Gangdise metallogenic belt
冈底斯成矿带
1.
Early Himalayan mineralization on the southern margin of the Gangdise metallogenic belt, Tibet, China: Evidence from Re-Os ages of the Chongmuda skarn-type Cu-Au deposit;
西藏冈底斯成矿带南缘喜马拉雅早期成矿作用——来自冲木达铜金矿床的Re-Os同位素年龄证据
2.
Recent examination and assessment about the porphyry copper deposits in Gangdise metallogenic belt, southern Xizang have revealed that these porphyry copper deposits are highly prospective.
近年来在西藏开展的资源评价和研究工作初步揭示出冈底斯成矿带斑岩铜矿床具有巨大的资源潜力。
6) Gangdese metallogenic belt
冈底斯成矿带
1.
The search for porphyry copper deposits in the Gangdese metallogenic belt has made great advance since the beginning of the geological survey project.
自1999年开展地质大调查以来,冈底斯成矿带斑岩铜矿研究取得了重大进展。
补充资料：延冈
延冈
日本九州东部城市。位宫崎县五濑川三角洲中心。人口14万。面积287.4平方公里。1933年设市。古城下町。1923年设立日本氮肥厂，今为化学工业中心。有药品、化学纤维、化肥等工厂。在业人口的三分之二与化学工业有关。有旧城遗址、九州第一瀑布（行膆瀑布，高110米）等旅游地。
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