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The Ulan Uzhur copper deposit, situated on the western margin of the Qaidam basin is a porphyry copper deposit controlled by granite porphyry dikes.

乌兰乌珠尔斑岩铜矿位于柴达木盆地西缘,为受花岗斑岩脉控制的斑岩型铜矿。

Haolibao copper-molybdenum deposit is of hydrothermal vein and porphyry type related to the Yanshanian crypto-explosive breccia-plagioclase granite porphyry and cataclastic sub-quartz-porphyry.

好力宝铜钼矿床属与燕山期隐伏的隐爆角砾状斜长花岗斑岩和碎裂次石英斑岩有关的热液脉状和斑岩型矿床。

40Ar/39Ar data of quartz from the granite porphyry and from the quartz veins in the granite porphyry range from 187.87±1.53Ma to 244.88±2.48 Ma, indicating products of structural hydrothermal fluids of Late Hercynian, Indosinian or Early Yanshanian perods.

花岗斑岩和花岗斑岩内的石英脉体中石英样品的40Ar/39Ar年龄数据表明户,40Ar/39Ar坪年龄值在187.87±1.53 Ma至244.88±2.48 Ma之间,是加里东期花岗斑岩成岩作用之后,海西、印支或者燕山早期多期构造热液作用的产物。

This study was only focused on the No.Ⅰore body. Based on detailed logging and dating results, it is considered that mineralization of the Cu_Au porphyry occurred in Late Jurassic. The formation of the ore body is related to the Late Jurassic augen quartz phenocryst_bearing hornblende_quartz diorite porphyrite intrusion(J3δομ).

通过对雄村铜金矿床Ⅰ号矿体详细的地质编录和测年成果,发现雄村斑岩型铜矿床形成于晚侏罗世,矿体的形成与晚侏罗世侵位的、含眼球状石英斑晶的闪长玢岩(J3δομ)有关,成矿岩体呈不规则的岩枝状,全岩矿化,岩体中Au的平均品位大于1g/t,Cu含量大于0.7 %。

The ore-forming materials were mainly derived from the volcanic rocks, the spilite providing quite more Cu, and the quartz keratophyre providing quite more Pb, while the spilite, keratophyre, and quartz keratophyre possibly providing quite more Au and Zn.

成矿物质主要来源于火山岩,其中细碧岩可能提供较多的Cu,而石英角斑岩可能提供较多的Pb,Zn的来源则相对较广,细碧岩、角斑岩、石英角斑岩均提供较多的Au。

On the basis of the metallogenetic theory of the porphyry deposit s,conception and deposit modeling from China and foreign geologists,the space-time characteristics of China porphyry deposit distribution,lithogenous and metallogenetic series,deposit types as well as regional composite model are discussed in this paper.

根据中外地质学家关于斑岩矿床的成矿理论、概念和矿床模式,论述了中国斑岩矿床分布的时空特点、成岩成矿系列、矿床基本类型和区域组合模式、区域和矿床成矿特征,是一份研究、寻找斑岩型矿床可遵循的资料。

The Himalayan (53.02 Ma) porphyries are superimposed upon the Indosinain Porphyries and seem to be closely related to copper mineralization.

喜马拉雅期(53.02Ma)斑岩叠加於早期的斑岩体之上,与斑岩铜矿化关系密切。

In this his dissertation, the field geological work and modern analysis were finished on the Qulong ore-bearing porphyries. The mineralization chronology, petrology, element and isotopic geochemistry were studied on the porphyries. This dissertation also compare this work in Qulong ore-bearing porphyries with other ore-bearing porphyries in Gangdese belt, in order to probe into dynamical background and mineralization features of the ore belts in the condition of India-Eurasia collision.

在充分搜集、利用前人资料及成果的基础上,本论文力求以地球动力学和现代成矿理论为指导,采用先进的分析测试手段和野外地质工作相结合的方法,通过重点研究驱龙斑岩铜矿床的岩石学、同位素地球化学、常量与微量元素地球化学及成矿年代学,并与冈底斯其它斑岩矿床对比,探讨在印度—欧亚大陆碰撞条件下,冈底斯斑岩铜矿带的大陆动力学背景及成矿规律。

The Permian dike rock is great development at Kuruktag Region, their rock association is diabase-tjositeplagiophyrite-granite-porphyry, among them, diabse is the most main rock type.

库鲁克塔格地区二叠纪脉岩群非常发育,主要岩石类型是辉绿岩,并有少量的斜闪煌斑岩、斜长玢岩和花岗斑岩。

There are two stages of ore formation in this region: skarn type Cu-Fe deposits; quartz vein and porphyry types Mo deposits, mainly is porphyry type, and both of them are the products of postmagmatic-thermal fluid.

该区存在两期成矿:Ⅰ期形成矽卡岩型Cu-Fe矿体;Ⅱ期形成斑岩型和石英脉型Mo矿体,以斑岩型为主。两期成矿均为岩装期后热液的产物。

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