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片岩

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Under arock,bravely Tanchunaodai grass,tenacious instinct for survival that it embraced the sun..people are often the case,the face of adversity and stress,often produce forward momentum.

片岩下的一棵不屈地探出脑袋的小草,求生的本能使它顽强地拥抱阳光…人也往往云云,在逆境和压力中,每一每一会孕育发生进步的动力。

Within the belt ,the mid-late Proterozoic green-schists were ovethrust from south to north onto the late Paleozoic granitic batholith at a low angle.

中晚元古代浅变质的绿片岩系自南向北以低角度辗掩于晚古生代花岗岩基之上。

Cavelike dwellings built into soft rock dot the Cappadocia region of Turkey.

位于土耳其的似坑洞的住处建成到绵软的片岩圆点内Cappadocia的地域。

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〓。

Combined with the data from early investigations for glaucophane in the Zhangbaling area,and con...

结合前人对张八岭地区的&蓝闪石&的研究资料,并对比作者等对天山昭苏、库车地区和西藏羌塘地区的蓝闪石分析数据,认为张八岭地区并没有真正意义上的蓝闪石存在,张八岭群中&蓝片岩&是否存在以及是否经历低温高压变质作用需要进一步的详细研究。

Exposed rock strata range from the 1.7 billion-year-old Vishnu Schist of the Inner Gorge, to the pale caprock Kaibab limestone deposited 250 million years ago, to the 1 million-year-old black lava flows in the western canyon.

暴露岩层中,从1.7亿岁片岩他人的峡谷内,到帕莱盖层kaibab石灰石存入250万多年前,以100万英镑岁黑色熔岩流在西部大峡谷。

Biotite-bearing monzonitic quartz schist is parametamorphite with a zircon U-Pb age of 978±13 Ma.

黑云二长石英片岩为副变质岩,锆石U-Pb年龄(978±13) Ma。

The flow stress of typical mylonitic structure in UHP bimica schists is Δσ=59.61 MPa.

超高压二云母片岩中石英典型的糜棱结构代表的差异应力为:Δσ=59.61MPa。

Dynamical metamorphism under greenschist facies is the condition of mineralizing enrichment.

绿片岩相以下的动力变质作用是矿化富集的条件。

As for epidotesfrom blueschist, X_=0.22--0.36, and their composition varies remarkablyeven.in the same sample. In general, fine--grained epidotes contain relativelylow ps while things are just the opposite for coarse--grained ones whichcommonly exhibit zonal structure characterized by the gradual decrease of pstowards the core, suggesting that the bluescbist might have experienced apressuree--decline metamorphic process.

s=0.22—0.36,其成分在同一样品中也有很大变化,一般细粒者ps分子少,而粗粒者ps分子多,且常发育环带结构,向中心ps分子减少,说明蓝片岩可能经历了一个以降压为特征的变质过程。

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