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mica schist相关的网络例句

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与 mica schist 相关的网络例句 [注:此内容来源于网络,仅供参考]

The eclogite lies in about 20 km east to Gemuri,Gerze county,Tibet.Eclogites occur as lenses and blocks of various sizes within the high-pressure metamorphic belt comprising garnet - muscovite schist and glaucophane - muscovite schist.

榴辉岩出露点位于西藏改则县戈木日东约20km,龙木错—双湖缝合带的中部,岩石呈透镜状、块状产在石榴白云母片岩和蓝片岩构成的高压变质带中,直接同岩为石榴白云母片岩。

Grand Canyon precipice on the bare rock era of large-span, both formed 20 million years ago schist Vishnu (Vishnu Schist, located in Inner Gorge at the bottom), and 2.3 billion years ago formed the limestone Keba (Kaibab Limestone, located on the shore).

大峡谷崖壁上裸露的岩层年代跨度很大,既有20亿年前形成的毗湿奴片岩(Vishnu Schist,位于 Inner Gorge 底部),又有2.3亿年前形成的凯巴灰岩(Kaibab Limestone,位于岸上)。

Based on the analysis of chemical composition,mineral composition and the spectral absorption characteristics of different lithostratigraphic units,the Relative Absorption BandDepthand the bandsratio method were adopted to process ASTER VisibleNear Infraredand ShortwaveInfraredmultispectral data from the east Kalpin Uplift,southwest Tian Shan. Limestone,dolomite,sandstone,blueschist/greenschist and psammitic schist/pelitic schist,in the study area were well discriminated.

基于新疆天山西南缘柯坪隆起东部不同地层单元岩石的化学组成和矿物成份以及VNIRSWIR谱域光谱吸收特征的分析,我们采用相关吸收波段深度和波段比值方法对研究区的多光谱遥感数据进行图像处理,有效区分和识别了白云岩、石灰岩、砂岩以及阿克苏群的蓝片岩—绿片岩和砂质片岩。

Results The creep characteristics, the isochrounous stress-strain characteristics and an empirical formula from creep curve of mica-quartzose schist have been obtained under the condition of the axial stress vertical to the direction of the schistosity surface.

结果 得到了当轴向力垂直于片理方向加载时,云母石英片岩的蠕变特性、等时应力应变特性和蠕变经验公式为σ1-σ3=178e(上标-0.0013t)ε1(上标 1.22e-0.0005t)和σ1-σ3=58.70e(上标-0.0071t)ε1(上标 1.67e-0.0068t)。

Below 1100℃, the amount of argon released from irradiated samples is in an order of: plagioclase rock>striped migmatite>granite>garnetiferous mica schist>calciummuddy shale>basalt.

在1100℃之前,辐照样释放的氩气量按顺序排列为:斜长岩>条带状混合岩>花岗岩>含石榴石云母片岩>钙泥质页岩>玄武岩。

The experiment results can give some benefit reference to establishing triaxial creep model of mica-quartzose schist.

所获得的经验公式为建立云母石英片岩的三轴流变模型提供了有益的参考。

Firstly, triaxial compression creep tests with mica-quartzose schist which is a kind of soft metamorphic rock with lots of schistosity surfaces were carried out on the rock servo-controlling rheology testing machine under the condition of the axial stress vertical to the direction of the schistosity surface.

首先,对片理发育的软弱变质岩—云母石英片岩,在轴向力与片理垂直的条件下,采用岩石全自动流变伺服仪进行了三轴压缩蠕变试验,对轴向蠕变和径向蠕变进行了对比分析,提出径向蠕变比轴向蠕变敏感,以径向蠕变长期强度作为长期强度更合理。

The quartz in this region shows a array of deformations from High-temperature -High pressure condition to crust environments: coesite → the high-temperature quartz → sheared quartz vein → feldspathic shear zone (the quartz from two-mica schist)→ the ordinary quartz in eclogites.

7本区石英的变形构成了一个从高温高压到中上地壳的连续变形序列:柯石英→榴辉岩中高温石英→剪切石英脉→长英质剪切带(超高压二云母片岩中石英)→榴辉岩中普通静态重结晶石英。

All rocks release large fraction of argon between 300 and 700℃ except garnetiferous mica schist. The amount of argon released between 700 and 1100℃ has a positive relation to Ca/K value on the whole. The saturation implantation dose of rocks in this experiment is~10〓 ions/cm〓.

除含石榴石云母片岩氩放气峰在900℃以外,其它岩石都在300-700℃放出大部分氩气,所有岩石在1100℃以下都释放了其中大部分的氩气。700-1100℃放出的氩气量基本与Ca/K呈正相关关系。120keV氩离子注入多种岩石的饱和剂量为~10〓粒子/cm〓。

It is concluded that because the mica schist is mixed with feeble weathered granite, the grain is broken up severely; the back-analysis parameters of explosion rockfill(3BⅠ)are lower than the results of laboratory triaxial test, and the Duncan E-B parameters obtained by back-analysis of her sandy gravel (3BⅡ)are higher than the triaxial test results of laboratory triaxial test which can not reflect the mechanical behaviors of the dam material objectively; the research should be strengthened in 300 m high rockfill dam construction. The fitting modes of the space displacement field of prototype observation are also explored and it turns out that the results of IGA analysis considering only vertical deformation meet the need of dam's technical accuracy.

结果表明,由于在微弱风化花岗岩掺加云母片岩,颗粒破碎严重,爆破堆石料(3BⅠ)的原级配粗粒料反演参数远低于室内三轴试验成果;与3BⅠ堆石料相反,砂砾料(3BⅡ)现场反演得到的邓肯E~B模型参数高于室内三轴试验值;室内三轴试验成果不能客观反映筑坝材料的力学特性,对于当今的300 m级高土石坝建设,宜加强对原级配粗粒料的力学特性研究;同时对原型实测的空间位移场不同拟合方式进行了探讨,认为仅考虑铅直向变形的IGA参数反演成果能基本满足土石坝工程的精度要求。

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