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Sm-Nd and Rb-Sr isotope data for amphibolite of the Bayanduxi Group, Inner Mongolia, China, are presented in the paper.

白银都西群主要由斜长角闪岩、变粒岩、长英片岩和条带状混合岩组成,是白银都西-白乃庙地体的重要组成部分[1,3],主要分布在内蒙古白乃庙铜矿床东北白银都西一带。

Mainly gneiss,mica schists,green schists and a little bit of granite.

主要是片麻岩,云母片岩,绿片岩及少量的花岗岩。

Among other things, the protolith of mica schist is claystone, those of quartz schist and granulitite are graywacke or subgraywacke and those of amphibolite, hornblende schist and garnet amphibolite are basic volcanic rocks.

斜长角闪岩、角闪片岩和榴闪岩的原岩为基性火山岩。

They are clay, mud shale, gravel, oil shale, mudstone, schist, basalt, limestone, gritstone, dolomite, breccia, granite, and quartzite. We give the feature curve and distribution feature equation of these rocked landslide.

本论文分别对不同滑体岩性,包括从软到硬的粘土、泥页岩、砾类土、油页岩、泥岩、片岩、玄武岩、灰岩、砂岩、白云岩、角砾岩、花岗岩、石英岩十三种具有代表性的岩土体的滑坡推力和剩余抗滑力进行了模拟分析,给出了它们的滑坡推力和剩余抗滑力分布特征曲线,分布特征方程。

After the deformation will enlarge the fine grains of the mylonite and at the same time will produce some new minerals. Thus, this will turn the mylonite into various crystallined schist.

随着片形后重结晶的增高,糜棱岩中的细小颗粒因重结晶而增大,并有一些新生矿物出现,使糜棱岩转变形成各种结晶片岩。

Through geothermometry and geobarometry, the temperature and pressure conditions of the three types of amphibolites are calculated, gneissic amphibolites: 597.0℃,0.536Gpa, banded amphibolites: 597.0℃,0.536Gpa, mylonitic amphibolites: 597.0℃,0.536Gpa.

通过地质温压计计算,三种斜长角闪岩及其原岩的形成与变形温压条件具有从升温升压经降温升压到降温降压的变化规律(片麻状斜长角闪岩:597.0 ℃,0.536 Gpa;条带状斜长角闪岩:597.0 ℃,0.536 Gpa;糜棱状斜长角闪岩:597.0 ℃,0.536 Gpa)。

Through geothermometry and geobarometry, the temperature and pressure conditions of the three types of amphibolites are calculated, gneissic amphibolites: 597.0℃, 0.536 GPa, banded amphibolites: 617.3℃, 0.455 GPa, mylonitic amphibolites: 558.8℃, 0.514 GPa.

通过地质温压计计算,3种斜长角闪岩及其原岩的形成与变形温压条件具有从升温升压经降温升压到降温降压的变化规律(片麻状斜长角闪岩:597.0℃,0.536 GPa;条带状斜长角闪岩:617.3℃,0.455 GPa;糜棱状斜长角闪岩:558.8℃,0.514 GPa)。

The ultra-high pressure metamorphic rocks distributed in the southern Dabie Shan have different rocks types including eclogites, garnet pyroxenite and garnet peridotite, quartz jadeitite, acid gneiss, phengite- quartz schist and marble.

分布于大别山南部的超高压变质岩具有丰富的岩石组合,主要岩石类型有榴辉岩、石榴辉石岩和石榴橄榄岩、石英硬玉岩、酸性片麻岩、多硅白云母石英片岩及大理岩等。

And later it was overprinted and reformed by the brittle structure and formed a complex ductile-brittle ...

在该带内已发现六个金矿体,赋矿围岩为蚀变的绿片岩、糜棱岩化碎裂岩和花岗质碎裂岩

The Laojunmiao metamorphic complex, exposed on the northeastern margin of the Junggar basin,consists mainly of quartz schists of greenschist facies, with some marbles bearing pre Devonian tabulates and crinoids resting on it.

出露在准噶尔盆地东北缘的老君庙变质岩,主要由绿片岩相的石英片岩构成,其上残存含前泥盆纪床板珊瑚和海百合茎化石的大理岩。

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