1) Baogutu porphyry copper deposit
包古图斑岩铜矿
1.
5)in Baogutu porphyry copper deposit have been tested by ASD and PIMA.
利用ASD和PIMA反射光谱测试仪对新疆西准噶尔包古图斑岩铜矿Ⅱ号、Ⅴ号斑岩铜矿岩体的蚀变围岩(地表采样与钻井采样)进行测试,并对结果进行分析总结。
2) porphyry copper deposit
斑岩铜矿
1.
Deep tectono-magmatic setting for metallogenesis of large porphyry copper deposits;
大型斑岩铜矿成矿的深部构造岩浆活动背景
2.
The latest advances in researches on porphyry copper deposits;
斑岩铜矿若干问题的最新研究进展
3.
Discovery of Jiru porphyry copper deposit in Tibet and its significance;
西藏吉如斑岩铜矿床的发现过程及意义
3) porphyry copper
斑岩铜矿
1.
Geological characteristics and genesis of the Ulan Uzhur porphyry copper deposit in Qinghai;
青海省乌兰乌珠尔斑岩铜矿床地质特征与成因
2.
Synthetic information prediction of porphyry copper in Tibet;
西藏冈底斯斑岩铜矿综合信息预测
3.
Quantitative assessment of the resource potential of porphyry copper systems in China;
中国大陆斑岩铜矿资源潜力定量评价
4) porphyry copper deposits
斑岩铜矿
1.
The ages, natures and tectonic environments of the Bangong Co porphyry copper belt have been preliminarily determined through a study of ore-bearing porphyries in the Dobuzha and Garqiong porphyry copper deposits in the porphyry copper belt.
通过对藏西班公湖斑岩铜矿带多不杂和尕尔穷2个大、中型斑岩铜矿床含矿斑岩的研究,初步查明了该铜矿带的形成时代、含矿斑岩性质及成矿构造环境。
2.
Zhongdian is enriched with indo-Chinese epoch neutral acid porphyry as well as one of the porphyry copper deposits in china that was an important breakthrough in the past few years.
中甸地区是印支期中酸性斑岩集中分布区,也是我国近年来寻找斑岩铜矿取得重大突破的矿集区之一。
6) porphyry copper deposit
斑岩型铜矿
1.
In the north- west and the south- east of Wuyi uplift inNanling minerogenetic area there exists respectively in each side of it a copper polymetallogenetic belt, including the famous porphyry copper deposits at Dexing and Zhijinshan which are related to intermediate-acid igneous rocks of Mesozoic Era.
南岭成矿区武夷隆起的北西、南东两侧各有一个铜多金属成矿带，其中包括德兴、紫金山等与中生代中酸性岩有关的著名斑岩型铜矿床。
2.
Dexing Copper Mine in Jiangxi province is the biggest open-pit non-ferrous metal mine in China,and it is a porphyry copper deposit.
江西德兴铜矿是我国最大的有色露天金属矿,属斑岩型铜矿山。
3.
This paper presents the morphological feature of the ore bodies in Shaxi porphyry copper deposit by means of trend analysis and with the help of computer program.
本文试图以数学（主要是统计数学）推演和计算机图形显示相结合的手段，对安徽沙溪斑岩型铜矿床多年来勘探成果的数据进行合理的归纳分组，应用趋势分析方法揭示了沙溪斑岩型铜矿体的空间形态在不同构造部位的变化特征。
补充资料：斑铜矿
| 斑铜矿 bornite 铜和铁的硫化物（Cu5FeS4）矿物，含铜量 63.3％，提炼铜的主要矿物原料之一。为四方晶系，其高温变体为等轴晶系，称等轴斑铜矿。表面易氧化呈蓝紫斑状的锖色，因而得名。新鲜断面呈暗铜红色，金属光泽，莫氏硬度 3 ，比重4.9～5.0。常呈致密块状或分散粒状见于各种类型的铜矿床中，并常与黄铜矿共生。也形成于铜矿床的次生富集带，但不稳定，而被次生辉铜矿和铜蓝置换。在地表易风化成孔雀石和蓝铜矿。中国云南东川等铜矿床中有大量的斑铜矿。世界代表性产地是美国蒙大那州的比尤特，墨西哥卡纳内阿和智利丘基卡马塔等。 |
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