绿泥石

The Trimouns deposit, in the French Pyrénées, is one of the largest talc and chlorite exploitation in the world.

位于法国比利牛斯山的Trimouns矿床是世界上最大的滑石-绿泥石矿床之一。

The result shows that the main types of clay minerals are illite, smectite, kaolinite and chlorite.

这些粘土矿物主要由伊利石、蒙皂石、高岭石和绿泥石组成。

Clay fraction is dominated by illite and kaolinite with small proportions of smectite, chlorite and vermiculite.

粘粒组成主要为伊利石和高岭石，也有少量蒙皂石、绿泥石和蛭石。

Clay minerals in the surface sediments of the central and southern South China Sea are illite, smectite, kaolinite and chlorite and their average percent contents are in tune 47%, 19%, 17% and 16%.

南海中南部表层沉积物中的私土矿物组合类型为伊利石－蒙脱石－高岭石－绿泥石，含量平均值依次为47%、19%、17%和16%。

On the basis of comprehensive discipline research, the rocks subfacies and microfacies of hydrothermal rocks facies have been initially studied and the their characteristic have been come to conclusions frist time.

在多学科综合研究基础上，首次系统提出研究并总结了热水沉积岩相的亚相及微相特征，亚相包括有：钠长岩-似碧玉岩亚相、硅质白云岩→硅质岩亚相、碱性钠长石质-碳酸质岩亚相、铁镁碳酸盐岩亚相、重晶石岩亚相、黑云母方柱石岩/黑云母岩亚相及铁绿泥石岩亚相。

The Shengmikeng vein-type lead-zinc deposit is located in Huanggangshan volcano-tectonic depression of the Mesozoic volcanic belt in Northern Wuyi.The ore featured by veinlets and disseminations is hosted both inside the fault zone in the upper Jurassic Ehuling ignimbrite and the potassic trachyte porphyry.

摘 要：生米坑铅锌矿床位于北武夷中生代火山岩带的黄岗山火山盆地内，已知铅锌矿体呈脉状产于侏罗系上统鹅湖岭组流纹质熔结凝灰岩的断裂内，或呈细脉——浸染状分布于钾质粗面斑岩内，发育钾长石化、绿泥石化、硅化等蚀变。

Distribution of strongly sericite altered zone, chlorite altered zone, montmorillonitized zone and kaolinized zone within study area were defined by PIMA survey, and the declining orientation of temperature at which altered mineral formed were pointed out.

PIMA测量在研究区内确定了强绢云母化带、强绿泥石化带、强蒙脱石化带和高岭石化带的分布范围，并且指出了蚀变矿物形成温度降低的方向。

The coesite-diamond-bearing eclogite distributed in the northern part of the UHPM belt suffered three stages of metamorphism. The first stage is the Ep amphibolite facies metamorphism, which is represented by the paragenesis of phe+Qtz+Cro/Bar Bar+Ep+Ab occurred as inclusions in Grt and Omp; The second stage is the peak metamorphism of eclogite facies with mineral assembledge of Grt+Omp+Coe±Dia±Ky±Zo±Phe+Rt. The P -T condition is 800±50℃,≥28Kb; The third stage is the amphibolite facies retrograded metamorphism from the peak one, which can be divided intothe early amphibolite facies stage with the mineral assembledge of Amp+ Pl+Di+Qtz±Ep+Ilm/Ttn and the late greenschist facies one with the mineral assembledge of Ep+Chl+Bi+Tr+Ab.

分布于超高压变质带北侧的柯石英榴辉岩经历了3个阶段的变质作用：(1)早期绿帘—角闪岩相阶段，以出现在石榴石和绿辉石中的包体矿物多硅白云母、石英、冰蓝闪石或青铝闪石、钠长石等为代表；(2)峰期柯石英榴辉岩相阶段，其矿物组合为Grt+Omp+Ky+Phe±Zo+Coe±Dia+Rt，其变质温度压力为800±50℃，≥28Kb；(3)退化变质作用阶段，早期为角闪岩相，以Amp+Pl+Di±Ep+Qtz+Tit等退变矿物组合为代表；晚期为绿片岩相，以绿帘石、绿泥石、黑云母、透闪石及钠长石等矿物为代表。

The strain JXF-1 had the maximum efficacy of releasing silicon in the tested strains from different resources, it can release respectively silcon 50.4% and 65.3% from raw bauxites and artificial mixed chlorites, but for strain B.

其中JXF-1菌株脱硅效果最好，可以浸出铝土矿原矿、绿泥石人工混合矿样中50.4%与65.3%的硅，而B.C菌株对该两种矿样的脱硅率仅分别为35.3%，48.2%。

The formation of high-grade ore body has undergone a complex process.

在复杂的成矿过程中，矿床所形成的地质构造、地球物理及地球化学等特征构成清晰的找矿要素，从不同尺度和有效性的要素系统，构建出以&中基性钙碱性火山碎屑岩+高极化高重力+多级复杂褶皱构造+硅化-绿泥石化+孔雀石化&为核心的矿床综合找矿模型。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。