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Major conclutions from this study can be summarized as following:1. On mineralogy, rutiles, apatites, epidotes and vein minerals from UHPM rocks were firstly and systematically studied, by detailed petrography and mineral-chemistry investigation, some mineral or mineral assemblage with special composions or texture were firstly found in UHPM rocks from Sulu-Dabie, for example, corrudum, magnesite, high-Ti biotite and garnet were found as inclusions in rutiles from eclogites, Nb-Fe rutile and zoned Si-Y apatite were found in gneiss, epidote / allanite with euhedral zones like magmatic genesis were found in elogites and gneiss, a lot of minerals with high REE, HFSE, LILE and volatiles were found in veins of gneiss.

在矿物学方面,首次较为系统地研究了超高压变质岩中的金红石、磷灰石、绿帘石等副矿物,并通过详细的岩相学和矿物化学研究,首次在苏鲁-大别超高压变质岩中发现了一些具有特殊成分/结构的矿物或矿物组合,如在榴辉岩金红石中发现了刚玉、菱镁矿、高钛黑云母和石榴石矿物包裹体,在片麻岩中发现了Nb-Fe金红石和具有自形环带结构的高Si-Y磷灰石,在榴辉岩和片麻岩中发现了具有类似岩浆成因的自形生长环带结构的绿帘石/褐帘石,在片麻岩的脉体中发现了大量富含稀土元素REE、高场强元素HFSE(Nb、Ta、Zr、Ti)、大离子亲石元素LILE(K、Th、U、Sr、Ba),以及挥发性组份(CO_2、F、P、S)的特殊矿物,丰富并提升了超高压变质岩的矿物学研究。2。

The rutile-hosted rocks are metamorphic rocks with amphibolite facie, but more work should be done to discuss features of their protolith.

这一化学特征显示了与岩相学观察相一致的结果,即富含金红石的岩石为透闪石含量偏低的直闪岩类。

Bismuth minerals and their relationship with gold mineralization are studied by means of reflect light microscope and electron probe microscope.The results show that bismuth, bismuthinite are main bismuth minerals in the two mines.

矿相学鉴定和电子探针分析结果表明,两矿床中的铋矿物以自然铋、辉铋矿为主,其次为碲铋矿、硫铜铋矿、辉铋铅矿等;铋矿物作为主要载金矿物,与自然金紧密共生;包村矿区Bi-Au相关系数为0.69,铋矿物与金矿化关系非常密切。

Under the theory of regional metallogenic system, this paper, focusing on Gaize district in Tibet, conducted carefully research in geological structure, magma activity, geophysical anomaly, geochemical anomaly, gold-bearing geological bodies and gold occurrence state, association of gold with other related elements, characteristics of typical deposits, metallogenic age, metallogenic process, post-ore-forming destruction of deposits in Gaize district based on methods of geology, petrology, economic geology, genetic mineralogy, isotopic chronology, geophysical and geochemical prospecting, and remote sensing.

本论文以藏北改则地区为重点研究区,以区域成矿系统理论为指导,采用地质学、岩石学、矿床学、成因矿物学、同位素年代学以及物、化、遥相结合的方法,对改则地区的地质构造、岩浆活动、物化遥异常、各地质体的含金性及金的赋存状态、金与相关元素的组合特征、典型矿床特征、成矿时代、成矿过程及矿床形成后的破坏作用等进行了较详细的研究。

These two ores have contrasting mineral associations: anthothyllite + plagioclase + rutile + magnesiohornblende + alkline fledspar for red ore and anthothyllite + phlogopite + epsode + Rutile for black ore.

根据岩相学观察,认为红色金红石矿中存在如下方向的反应:镁角闪石+碱性长石→直闪石+/-斜长石+/-金云母,斜长石很可能只是过渡相,反应最终将形成直闪石+金云母。

In this 'TWSSG Premium Event in Japan' casts of MBC drama 'TWSSG' including BYJ, Moon Sori, E Ji Ah, Park Seongwoong, Lee Phillip, Oh Kwangrok, etc, and Kim Jonghak PD, who directed it, will attend.

"'太王四神记'日本宣传活动"期间,这部韩国MBC电视台录制的电视剧中的主角裴勇俊、文素利、李智雅、朴相元、崔明洙等以及导演金钟学将到场。

The fluid inclusion petrography and homogenization temperature of quartz vein type Au ore and the altered cataclastic rock type Au ore (area 210) show different characteristics of the fluid inclusions and variation of the ore-forming temperatures. The fluid inclusions can be divided into Ⅰ and Ⅱ types, i.

通过对北山地区金窝子矿区石英脉型金矿和210矿区蚀变岩型金矿中流体包裹体的岩相学和显微测温研究,查明了不同金矿类型中流体包裹体的特征和成矿温度的变化特征。

Basing on detailed field survey and laboratory researches on lithological features, mineralogical composition, geochemical and zircon SHRIMP U-Pb data, together with the mineralogical study of chromitite and mantle peridotite heavy mineral bulk sample, various proceedings and recognitions have been achieved:(1) The mantle peridotite is the remnants of partial melted MOR mantle altered by SSZ fluids.

通过详细的野外调查和室内岩石薄片的岩相学、矿物成分、岩石地球化学和锆石SHRIMP U-Pb同位素年代学,铬铁矿和地幔橄榄岩的人工重砂大样的矿物学研究,取得以下进展和认识:(1)认为康金拉地幔橄榄岩为部分熔融MOR地幔残余,叠加了SSZ流体的改造。

Knowledge of metallographic analysis and material inspection methods.

具有一定的金相分析学和金属材料检测方法的知识4。

The creation of metallography haa been started with microscopic study of metallic samples,and discoveries 01 micros tructure within metallic materials.

金相学的创立始于人们在显微镜下研究金属样品并发现了金属材料的显微组织。

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