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岩化

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Migmatization in Higher Himalayan Crystallines resulted from anatexis that took place at 22.67(/-0.60) Ma.

3高喜马拉雅结晶岩系的混合岩化现象是地壳深熔作用的结果。

The MT carbonates formed several stages and with complex origin, special in dolomitization, MT carbonate was in the form of calcite in epigenetic stage; This is the preliminary research fruit.

MT的形成具有多期性和复杂成因,在白云岩化中也有分布,MT在后生白云岩中依旧以方解石形态存在,这是初步研究成果。

The rock is chiefly marked by mixing of blocks of various ophiolite components of varying size and nature in mylonized matrix.

主要表现为糜棱岩化的基质中混杂着大小不一、性质各异的蛇绿岩各组分的岩块。

With the exception of rare, relatively well-preserved Phanerozoic shells, this happens to all carbonates.

排除那些稀少的,相对保存完好的显生宙shells,这种所谓的岩化过程基本会发生在所有的碳酸盐岩中。

Fault rocks, microstructures and homogeneous temperature (concentrated around 160℃) of fluid inclusions in the quartz veins shows that the fault belt mainly underwent shallow brittle deformation and the highest-grade dynamic metamorphic rock is mylonitized sericite phyllite.

显微构造、断层岩与石英脉流体包裹体均一温度(集中在160℃附近)均显示,断裂带以浅层脆性变形为主,最深动力变质岩仅为糜棱岩化绢云母千枚岩。

The matrix consists dominantly of mylonized volcanic rocks, tuff and strongly fragmented pyroclastic rocks.

基质主要有糜棱岩化的火山岩、凝灰岩和破碎强烈的火山碎屑岩。

The most frequent reaction causing the self-sealing of rocks with high secondary permeability is argillization.

这种发生频率很高的、使次生渗透性能良好的岩体产生自封闭现象的反应就是泥岩化

Calculations based on Grosens'component-volume equation show that,wit the intensification of mylonitization,increasing amounts of SiO_2 and FeO are brought in,which is geologically expressed as intensified silicification and pyritization.

根据Gresens的成分-体积关系式所获得的计算结果表明:SiO_2、FeO随着糜棱岩化程度加强而带入量增加,在地质上表现为硅化、黄铁矿化加强

Calculation of loss and gain of components in parentage and altered rocks during metasomatism, reveals that, in rubification and afforestation belts, the components brought in were K〓, CO〓, H〓O, and the components brought out were SiO〓, Ca〓 and Na〓, implying that the early ore-bearing hydrothermal fluids were rich in CO〓 and H〓O. SiO〓 brought out from potassic and chlorite alteration zones could serve as the main source for SiO〓 necessary in the formation of quartz veins, of silicification and of bericitization at shallow depth.

说明早期成矿流体为富含CO〓、H〓O等的碱性流体,其中钾化、绿化带中带出的SiO〓等是浅部石英脉、硅化、绢英岩化中硅质的主要来源,带出的Ca〓与成矿流体中的CO〓结合形成碳酸盐化,带出的Na〓则在浅部形成钠长石脉。

Therefore, the mudstone is rigidly hard in the dry state, but it swells and slakes easily when it absorbs water.

我国西南部泥岩由於成岩时间短、岩化程度低,乾燥时坚硬如石,遇水则易生回胀、崩解。

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