淡色岩

The large volume of garnet granite is possibly direct products of anatexis of the Khondalite series, which is indicated by their feldspar Pb composition consistence and some petrological evidences.

花岗岩中长石Pb同位素组成显示，石榴石花岗岩是孔兹岩系部分熔融的直接产物，而淡色花岗岩不是孔兹岩系简单的部分熔融产物。

The leucogranites veins occurred widespreadly in the para-metamorphic rocks, in which the hypersthene melagranulite distributed. That suggests the source rocks of leucogranites of the High Himalaya are para-metamorphic rocks. For the basement was uplifting, pressure relieved and lacked water, source rocks were melting partly and formed the leucogranite magma.

基底副变质岩中广泛分布淡色花岗岩脉体，在基底副变质岩中的淡色花岗岩脉体中发现紫苏辉石暗色麻粒岩残留体，这表明本区高喜马拉雅淡色花岗岩源岩为基底副变质岩，且基底副变质岩是在基底快速隆升降压的条件下发生缺水熔融生成的淡色花岗岩岩浆。

These dilatation veins are the ultramafic—mafic intrusive sheets in early stage, which occurred the strong boudinages and the shearing rotation forming θ、Φ、δtype porphyroclasts generally, as the series different size deformation zones; the features of the leucocratic felsic veins in middle stage; the pink granitoid veins in later stage, show a gneisses evolution process from the deep tectonic facies to the middle tectonic facies.

这些扩张脉体，早期阶段为超镁铁质—镁铁质侵入岩席，受后期构造改造岩席发生强烈石香肠化或受剪切发生旋转，呈θ、Φ、δ碎斑系，总体构成一系列规模不等的变形带；中期阶段以发育淡色长英质脉体为特征；晚期阶段为肉红色花岗质脉体，反映出片麻岩由深构造相向中浅构造相变化的过程。

The pluton contains olive gabbro, tint olive gabbro, tint gabbro, troctolite and gabbro, with olive gabbro and troctolite predominating.

该岩体主要由橄榄辉长岩、浅色橄榄辉长岩、淡色辉长岩、橄长岩及辉长岩组成，以橄榄辉长岩和橄长岩为主。

Above the Redwall come alternating layers of red sandstone and shale 1,000 feet thick, then comes the next pale-blue layer.

在&红墙&的上方，是红色的沙岩和1 000英尺厚的页岩交替层，然后是浅蓝色的沙岩层，最上层是淡**的石灰石。

Above the Redwall come alternating layers of red sandstone and shale 1,000 feet thick, then comes the next pale-blue layer.

在&红墙&的上方，是红色的沙岩和1 000 英尺厚的页岩交替层，然后是浅蓝色的沙岩层，最上层是淡黄色的石灰石。

Above the Redwall come alternating layers of red sandstone and shale 1,000 feet thick, then comes the next pale-blue layer.

在&红墙&的上方，是红色的沙岩和1 000 英尺厚的页岩交替叠层，然后是浅蓝色的沙岩层，最上层是淡黄色的石灰石。

Above the Redwall come alternating layers of red sandstone and shale 1,000 feet thick, then comes the next pale-blue layer. The topmost layers are a yellowish limestone.

在&红墙&的上方，是红色的沙岩和1 000 英尺厚的页岩交替层，然后是浅蓝色的沙岩层，最上层是淡黄色的石灰石。

Above the "Red wall" come alternating layers of red sandstone and shale 1,000 feet thick, then comes the next pale-blue layer. The topmost layers are a yellowish limestone.

在&红墙&的上方，是红色的沙岩和304.8米厚的页岩交替层，然后是浅蓝色的沙岩层，最上层是淡黄色的石灰石。

Above the Redwall come alternating layers of red sandstone shale 1,000 feet thick, then comes the next pale-blue layer. The topmost layers are a yellowish limestone.

在&红墙&的上方，是红色的沙岩和1 000 英尺厚的页岩交替层，然后8t t t8.com 是浅蓝色的沙岩层，最上层是淡黄色的石灰石。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。