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Basic Types of High-quality Clastic Reservoirs Deep-buried in Superimposed Basins in China.

中国叠合盆地深层有利碎屑岩储层的基本类型。

In the evolution of the foreland basin, 8km thick clastic rock was deposited.

在前陆盆地演化过程中,沉积了厚达 8km的碎屑岩。

In order to remedy this shortage, it was put forward that the frame of terrigenous elastic rocks should be expressed as the collaring rectangle instead of rectangle.

对于陆源碎屑岩来说,这样既不能表示出其粒度变化情况,又不能反映出它形成时的沉积动力学特征。

Today's coast is never clear but always strewn with plastic and other detritus .

今天的海岸不再空旷,但却四处散布着塑料品和其它碎屑。

In a word full of mind numbing media detritus it is easy to fall prey to speaking without taking action.

总之充分的考虑到麻木媒体碎屑很容易牺牲品发言没有采取行动。

In the fields of diagenesis study,there is few prevenient research on diagenesis of the volcano-sedimentary rocks.

在成岩作用研究领域,前人对火山碎屑—沉积岩的成岩作用研究较少。

The Es2-3 Member with buried depth more than 3500m in Banqiao-Beidagang area, consists of clastic rocks, develops a sedimentary system mainly containing deep-water turbidite fan,fan delta and alluvial digitate sand bar.

板桥—北大港地区深层(3500m以下深度)沙二段、沙三段发育以深水浊积扇、扇三角洲和冲积扇指状砂坝为主的碎屑岩沉积体系。

The basin sediments include volcaniclast and deep-water deposit from arc and terrigenous flysch deposit.

盆地沉积物包括来自岛弧的火山碎屑、深海沉积物和陆源复理石沉积。

The fossiliferous Middle Carboniferous and Permian are well developed in the Deri′angma-Xiala section in the Yunzhug area, Xainza County, northern Tibet.

西藏北部申扎县永珠地区德日昂玛-下拉剖面中石炭系和二叠系地层发育完整,出露良好,化石丰富。该剖面中查果罗玛组碳酸盐岩地层和下拉组碳酸盐岩地层之间的碎屑岩夹灰岩地层,在沉积上表现为冰海相杂砾岩,在古生物化石面貌上表现为特提斯-冈瓦纳古生物群混生。

The Laojunshan conglomerate is a suite of continental coarse clastic rocks consisting of conglomerate and graywacke.

老君山砾岩是一套由砾岩和杂砂岩组成的陆相粗碎屑岩。

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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。