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The shale, mudstone and limestone are not good for building.

侵入岩、火山碎屑岩和砂岩,坚硬致密,风化裂隙不发育,是很好的建筑基岩。

Wave-rippled ooid–intraclast grainstone beds and bedsets overlie shale or form the base of the second cycle type.

波痕状鲕粒内碎屑颗粒灰岩覆于页岩上或形成第二种旋回类型的底部。

Nadigangri formation mainly consisted of volcanic deposition, including continental effusive rocks, marine effusive rocks, and volcanc clastic deposition, which reflected the early paleography of rift basin.

那底岗日组主要为火山—沉积,分为陆上喷溢、水下喷溢和火山碎屑沉积,反映裂陷盆地早期的古地理面貌。

The Pana volcanic rocks of the Linzizong Group in Zhaxue area, Linzhou County, Tibet are mainly composed of rhyolitictrachy lavas and volcanoclastic rocks.

分布于西藏林周县扎雪地区的林子宗群帕那组火山岩,主要由流纹质-粗安质熔岩和火山碎屑岩组成。

And even yonger ages for inherited detrital zircons and magmatic zircons of paragneiss.

副片麻岩中包含了730Ma、680Ma、621Ma和较年轻的继承性碎屑锆石和结晶锆石年龄。

Most people can easily escape the lava flow, pyroclastic flow, but escape is not so easy.

人们可以轻易地躲开大部分的熔岩流,但躲避火山碎屑流却不那么容易。

Pyroclastic rocks are a kind of transitional and complex rocks between lavas and sedimentary rocks.

火山碎屑岩是介于熔岩和沉积岩之间的过渡类型岩石,岩类复杂。

The greatest dangers of pyroclastic avalanches are probably heat and suffocation.

火成碎屑崩落的最大危害可能是炽热和窒息作用。

It was yesterday I thought myself a fragment quivering without rhythmic in the sphere of life.

就在昨天,我还以为自己只是碎屑一片,在生命的苍穹之中毫无韵律地颤抖。

The problems arise because juvenile sandfish are deposit feeders and require large surface areas to forage for detritus and bacteria.

出现的问题,因为少年sandfish是存款馈线和需要大面积寻找碎屑和细菌。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。