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含岩屑
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  containing debris
     thedeformation of the basal layer containing debris contributes immensely to overall motion;
     冰川底部含岩屑层的变形对冰川运动的贡献显著;
短句来源
  “含岩屑”译为未确定词的双语例句
     Constant Stress Creep Experiments Ice Containing Debris of Glacier No.l at the Headwaters of the Urumqi River
     乌鲁木齐河源1号冰川含岩屑冰川冰的恒应力蠕变试验
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     The most commonly found sandstone is quartz-arenite with feldspar and rock fragments,the next,are lithic quartz-arenite with feldspar, quartz-arenite and feldspathic quartz-arenite, and the wackes are seldomly found.
     区内最常见的是含长石含岩屑石英砂岩,其次是含长石岩屑质石英砂岩、纯石英砂岩、长石质石英砂岩,杂砂岩很少。
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  相似匹配句对
     thedeformation of the basal layer containing debris contributes immensely to overall motion;
     冰川底部岩屑层的变形对冰川运动的贡献显著;
短句来源
     Chromium-containing phosphate
     铬的磷酸盐
短句来源
     MOLYBDENUM-CONTAINING LUBRICATION MATERIALS
     钼润滑材料
短句来源
     Constant Stress Creep Experiments Ice Containing Debris of Glacier No.l at the Headwaters of the Urumqi River
     乌鲁木齐河源1号冰川岩屑冰川冰的恒应力蠕变试验
短句来源
     CUTTING-GAS ANALYSIS
     岩屑气的测定方法
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  containing debris
They suggest that cholesterin containing debris entering the subarachnoid space from the tumour cysts provoke an aseptic "chemical" meningitis of short course.
      
The cytotoxic effects of the injected compounds on the peripheral and central nervous system were investigated by light and electron microscopy; the severity of CNS lesions was evaluated by quantitation of macrophages containing debris.
      
This correlation demonstrates that computer image processing provides opportunities for comparing root length parameters between different laboratories for samples containing debris.
      
A 1994 EPA regulation indicated that treatment standards for all mercury-containing debris in excess of 60 millimeters were to be suspended.
      
Forward and side scatters were used to gate out containing debris.
      
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Glacier No. 3 is a cirque type-compound glacier with a steep accumulation-ablation slope and a typical glacier in the area of the Urumqi river headwaters.

3号冰川从积累区到消融区坡度很陡,是一条复合型冰斗冰川。可谓之乌鲁木齐河源冰川的一个典型。 1981年夏季期间对冰舌区冰川结构特征、冰川末端和前缘冰碛垅的产生及性质、一定时期的物质平衡、新冰期时形成的终碛垅的形态等进行了观测。绘制出了冰舌区和终碛垅的详细地形图,并研究了岩屑聚积的污化带的详细结构。 对含有污化层的冰川冰进行了氧同位素含量和化学成分的分析。以这些结果为基础,可以推测污化带为一种剪切面,所含的岩屑系压力融化-再冻结过程中冰下冰碛所携带。

The coal-bearing Longtan Formation of Late Permian in Yangqiao mine area in Jiangxi province is composed of alternating marine-terrestrial deposits.The total thickness ranges from 403鈥?37m, and one fifth of the total thickness is sandstone. The most commonly found sandstone is quartz-arenite with feldspar and rock fragments,the next,are lithic quartz-arenite with feldspar, quartz-arenite and feldspathic quartz-arenite, and the wackes are seldomly found. The sandstone strata are composed of fine to very fine...

The coal-bearing Longtan Formation of Late Permian in Yangqiao mine area in Jiangxi province is composed of alternating marine-terrestrial deposits.The total thickness ranges from 403鈥?37m, and one fifth of the total thickness is sandstone. The most commonly found sandstone is quartz-arenite with feldspar and rock fragments,the next,are lithic quartz-arenite with feldspar, quartz-arenite and feldspathic quartz-arenite, and the wackes are seldomly found. The sandstone strata are composed of fine to very fine grains of sands, well sorted (grade I), and is sub-mature (grade III) to mature (grade II) in mineralogy. The major light mineral in rock is quartz and the minor ones are chert fragments and feldspar. The feldspars in rocks have been strongly illitized. The heavy minerals in sandstone are varied. being mostly zircon and tourmaline,which indicated that the clastic materials were resulted from physical desintegration and chemical decomposition under tropical climate conditions, and then were transported for long distance to littoral areas and finally deposited there.Zircon in sandstone of Shizishan member is colorless, pure in composition, well rounded and sorted, showing that it is of re-deposition origin. Ziron grains in sandstone of Guanshan member are flesh-red in color and have evidently rough surfaces and are well rounded, which are similar to characteristics of old granite- gneiss formation, and therefore, suggest that the parent rocks of the Guanshan member are possibly the old granites and gneisses in the central and southern Zhejiang province and northern Fujian province.

江西省杨桥矿区晚二叠世龙潭组含煤地层是一套海陆交互相沉积,沉积厚度在403m至437m,砂岩厚度占总厚度的五分之一。区内最常见的是含长石含岩屑石英砂岩,其次是含长石岩屑质石英砂岩、纯石英砂岩、长石质石英砂岩,杂砂岩很少。砂岩粒度以细砂级及微砂级为主,分选较好(Ⅰ级),矿物成熟度为准成熟(Ⅲ级)及成熟(Ⅱ级)。岩石中轻矿物以石英为主,次为燧石岩屑和长石,长石强烈水云母化。重矿物种类较多,但以较稳定的锆石和电气石为主,代表湿热气候条件下既有物理风化又有化学风化,碎屑物质经长距离搬运至滨海地区堆积的产物。狮子山段砂岩中锆石具有无色浑圆状,成分纯,分选和圆度较好,推测是再沉积成因的。官山段砂岩中含肉红色锆石,糙面显著,浑圆度好,具有古老的花岗-片麻岩建造的锆石特征,因此官山段砂岩的母岩可能是浙中南及闽北的古老的花岗岩和片麻岩。

A tunnel was excavated in the terminus of the east tributary of Glacier No. 1 at thehadwaters of the Urumqi River. Observations show that ice temperature is close to butslightly lower than the melting point;crystal size is quite large,with the mean diameter reach-ing ten odd milimeters;c-axis orientation mostly appears multi-maximum pattern; thedeformation of the basal layer containing debris contributes immensely to overall motion;and the terminus is an area of radical stress changing, with large strain, significantlongitudinal...

A tunnel was excavated in the terminus of the east tributary of Glacier No. 1 at thehadwaters of the Urumqi River. Observations show that ice temperature is close to butslightly lower than the melting point;crystal size is quite large,with the mean diameter reach-ing ten odd milimeters;c-axis orientation mostly appears multi-maximum pattern; thedeformation of the basal layer containing debris contributes immensely to overall motion;and the terminus is an area of radical stress changing, with large strain, significantlongitudinal compression and vertical rising;The principal strain rate is of the order of mag-nitude of 10~(-1)a~(-1).The elongation,shortening and rotation of the principal axes of strain el-lipses on the wall of the tunnel increase from the back wall towards the tunnel entrance.

在乌鲁木齐河源1号冰川东支末端开挖了2号冰洞。观测表明,冰温接近且略低于冰的融点;冰晶粗大,平均直径一般达十余毫米;大部具有多极大型组构;冰川底部含岩屑层的变形对冰川运动的贡献显著;冰川末端是一个应力剧变区,应变大,纵向压缩和竖向上升明显。主应变率在10 ̄(-1)a ̄(-1)的数量级。洞壁上应变椭圆主轴的伸长、缩短和旋转均自洞里向洞外增加。

 
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