斑岩铜矿床

  • 网络porphyry copper deposit
斑岩铜矿床斑岩铜矿床
  1. 斑岩铜矿床原生晕分带模式及其控制因素

    Zoning patterns of primary halos and their controlling factors in porphyry copper deposits

  2. 斑岩铜矿床研究综述

    A summary of researches on porphyry copper deposits

  3. 青海省乌兰乌珠尔斑岩铜矿床地质特征与成因

    Geological characteristics and genesis of the Ulan Uzhur porphyry copper deposit in Qinghai

  4. 然而,该斑岩铜矿床无确切的年代学数据。

    However , no precise chronological data are available about the porphyry copper deposit .

  5. 江西德兴斑岩铜矿床某些元素的扩散和渗滤作用

    Diffusion and infiltration processes of some elements in the Dexing porphyry copper deposit , Jiangxi

  6. 作为贱金属主要来源的斑岩铜矿床,大多数产出于大陆边缘和岛弧环境。

    Most porphyry Cu deposits , a main source of base metals , occur in continent and island-arcs .

  7. 中国东部斑岩铜矿床模式数据库处理系统及设计中几个问题的处理

    A data base processing system for porphyry copper deposits model in East China and several problems handling in programing

  8. 针对西部某一大型斑岩铜矿床矿石进行了选矿合理工艺流程和药剂制度的研究。

    Reasonable mineral processing flowsheet and regime of agent have been studied for the ores in a certain large porphyry deposit .

  9. 驱龙等大&超大型斑岩铜矿床的发现与评价,标志着一个超千万吨级的斑岩铜矿勘查开发基地已经初步形成。

    The Gangdise zone is also a porphyry metallogenic zone where a major breakthrough has been made in copper exploration in China .

  10. 羊鸡山金矿床与斑岩铜矿床系列各类铜矿床空间上密切相伴,处于同一构造&岩浆成矿带。

    The Yang - jishan gold ore deposit is intimately linked with various copper ore deposits of the porphyry copper ore deposit series in a structral - magmatic-metallogenetic belt .

  11. 以江西德兴斑岩铜矿床之细矿脉为研究对象,文章介绍了细矿脉剖面采集及研究的工作方法,着重讨论了自矿脉至围岩元素的空间展布特征。

    In the article , the ore veinlet of the Dexing porphyry copper deposit has been chosen as an object of study , the working method for the ore veinlet profiles has been introduced .

  12. 带内有超大型的德兴斑岩铜矿床、金山金矿床、银山多金属矿床以及许多中小型矿床,其中铜储量和伴生金储量分别占全国的17.5%和37%。

    The copper and gold reserves in the belt account respectively for 17 . 5 per cent of copper reserves and 37 per cent of gold reserves of associated gold deposits ( in which gold occurs as a valuable component in ores ) of the whole country .

  13. 中国斑岩型铜矿床品位&吨位模型

    The grade - tonnage model of the China porphyry copper deposits

  14. 斑岩型铜矿床地球化学勘查中岩石化学指标

    Petrochemical indices in geochemical exploration of porphyry type copper deposits

  15. 矿床地球化学特征、矿体特征均显示出斑岩型铜矿床特点。

    The geochemical and geological characteristics are the same a those of a porphyry copper deposit .

  16. 中蒙边境及邻区斑岩型铜矿床地质特征及成因

    Geological Features and Origin of Porphyry Copper Deposits in China - Mongolia Border Region and Its Neighboring Areas

  17. 该矿床可分为火山气液沉积铜矿床和斑岩型铜矿床两种类型。

    The copper deposits may be grouped into two types : the volcanic exhalative sedimentary copper deposit and porphyry copper deposit .

  18. 与酸性侵入岩有关的热液脉状型、矽卡岩型和斑岩型铜矿床,以及复合成因的脉状铜矿床。

    - related hydrothermal vein copper deposit , skarn and porphyry copper deposite as well as the vein copper deposit with complex origin .

  19. 公婆泉铜矿是北山地区最大的铜矿床,也是我国西北地区一个非常重要的斑岩型铜矿床。

    The Gongpoquan copper deposit is not only the biggest one in the Beishan area , but also a very important copper deposit in northwestern China .

  20. 依据1997年全国矿产储量数据库资料,对全国72个斑岩型铜矿床建立了品位模型、吨位模型以及吨&品位联合模型。

    The article has established grade-tonnage model to 72 porphyry copper deposits of the whole country , according to The Mineral Resources Data Base of the Whole Country .

  21. 本文首次概括综合信息三维找矿模型显示,该区可能赋存一个超大型斑岩系列铜矿床。

    According to the 3D prospecting model of comprehensive information put forward first in this paper , there is a potential super large porphyry Cu deposit maybe in this area .

  22. 斑岩铜矿中的绿泥石及其形成条件我国大陆东部斑岩型铜矿床成矿岩体的岩石化学特征及其成矿物质来源探讨

    Chlorites in porphyry copper deposits and their forming conditions petrochemical characteristics of COPPER-PRO ductive porphyries in the eastern part of China continent and their material sources

  23. DonJavier斑岩型铜矿床隶属秘鲁南部斑岩铜矿带,是典型的陆缘弧环境下的斑岩型铜矿床。

    The Don Javier porphyry copper deposit , part of porphyry copper belt in southern Peru , is a typical porphyry copper deposit in continental margin-arc environment .