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Actinolite and pyroxene phenocrysts separated respectively, from chlorite-actinolite schist and altered pillow basalt in the E'rou area of the eastern part of the Shuanghu-Longmuco suture zone, yield well-defined 40Ar/39Ar plateau ages of 235.9±2.6 Ma and 232.5±2.4 Ma. These nearly identical ages are interpreted as defining the age of the tectonothermal event of subduction-related collision along the Shuanghu-Longmuco suture zone.

在藏北龙木错-双湖缝合带东段双湖鄂柔地区,获得绿泥阳起石片岩中阳起石矿物的40Ar/39Ar坪年龄为(235.9±2.6)Ma和枕状玄武岩中蚀变辉石斑晶的40Ar/39Ar坪年龄为(232.5±2.4)Ma,两个年龄具有极好的一致性,记录了中三叠世晚期-晚三叠世早期沿龙木错-双湖缝合带发生俯冲碰撞作用的构造-热事件。

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)。

The Dagougu gold-bearing albitite, which is characterized by bedding and massive struc-ture, is mainly stratiform and 1enticular in shape, and also occurs as veins in the Late Proterozoicschist.

粤西大沟谷一带钢长石岩主要以层状、透镜状及脉状产于震旦系乐昌峡群变质片岩中,具块状及条带状构造,是大沟谷金矿的主要赋矿岩石。

The volcanic rock belt in Yushu has experienced strong contraction deformation,thus the green schist phase of low-degree metamorphism was widely developed and the fanlike nappe overlapped the tectonic units on both sides.

玉树火山杂岩带内岩石经历了强烈挤压和多层次的构造变形,普遍发生绿片岩相的浅变质作用,形成&扇状&推覆体叠盖在两侧构造单元上。

Nalaqi structure belt ; the time of the main strata ; the ophiolite and glaucophane schist ; the background of the formation of Dahala Junshan volcanic rock ; characteristics of the texture ; Xinjiang China

那拉提构造带;地层时代;蛇绿岩和蓝闪片岩;大哈拉军山火山岩系形成背景;结构特征;中国新疆

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)。

collision between the North China and Yangtze cratons.

这套岩石在印支期(约230 Ma)华北与扬子板块碰撞过程中经历了低温高压蓝片岩—榴辉岩相变质作用。

Yuntai Fm Kyanite Quartzite Schist Northern Jiangsu

云台群;蓝晶石;石英岩;片岩;江苏北部

Tectonic schists are formed by dislocation and new mineralization at the middle-high level of the crust, and consist of the syntectonic new minerals and matrix.

构造片岩系列形成于地壳中浅部构造层次上,以位错蠕变和新矿物化作用为主,由同构造新生片状矿物和基质组成。

The chlorite ores altered from mica schists are either massive or schisteous ores with gray greenish and dark gray colors.

而由云母片岩蚀变而来的绿泥石矿石呈块状或片理状、颜色为灰绿色和深灰色。

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