边石

In order to control blasting flyrock,improve blasting effect and stonework shovelling efficiency,shallow blasting and bench blasting were used to strip advance drift in blast area and southward and northward free face.

为了控制爆破飞石，改善爆破效果，提高石方铲装效率，在爆破施工过程中，爆破区超前导坑槽和南、北面剥离采用浅孔台阶爆破方法，边坡开挖轮廓线处采用光面爆破方法，严格按照爆破设计参数施工，取得了良好的爆破效果，可供类似工程参

A —Sample ZM641 , garnet porphyroblast with inclusionsof amphibole , epidote , plagioclase concentrated in the core of crystal , the rimof the garnet

a —样品ZM641 ，角闪石、绿帘石和斜长石包体分布在石榴石变斑晶核部，边部有绿辉石包体，基质矿物主要为绿辉石背散射电子图像

Talking while they walked, they finally arrived at a small stone hut and sat down on a bench in front.

三人边走边谈，这时已走到一个小石屋旁，三人便在屋前的凉椅上坐了下来。

At the edge of a dark crack in the ground stands the stone form of a dead gargoyle.

在地上一个黑乎乎的裂缝边，站着一个死亡的石像鬼所剩下的石体。

Day was at hand. I lit my lantern, and by its glow-worm light put on my boots and gaiters; then I broke up some bread for Modestine, filled my can at the water tap, and lit my spirit lamp to boil myself some chocolate.

天快亮了。我点上灯笼，借助着它的萤火虫般的微光穿上我的长靴和绑腿；然后给Modestine撕了几片面包，在溪石的水柱边灌满了水，点燃酒精灯煮了几块巧克力。

After traversing a hundred paces, skirting a wall of the fifteenth century, surmounted by a pointed gable, with bricks set in contrast, he found himself before a large door of arched stone, with a rectilinear impost, in the sombre style of Louis XIV., flanked by two flat medallions.

他走上百来步，到了一道十五世纪的墙脚边，墙上有用花砖砌的山字形尖顶，沿墙过去，便看见一扇拱形石库大门，一字门楣，配上两个圆形浮雕，具有路易十四时代的浑厚风格。

The deep water deposition means the deposition in the area where the water depth is larger than 30 meters, in which the major sediments are coarse sand and gravel. This kind of deposition is the relic deposition formed by the Pleistocene alluvial-lacustine deposition reworked under modern channel currents actions, and ususally the Holocene acummulation lack in the deep waters. The transitional zone deposition is the deposition between the low tidal level line and the 30 meters isobath, where the sediment types is changeable and the grain sizes are gradually coarsening from the low tidal line to the deep water area. This kind of deposition is developed by the deep water eroded sediments sorting under the transitional zone current action. The different types distributed along the isobath. The tidal flat deposition is the fine sediment deposition on the tidal flat which is flo sedimentation of the silty clay under the tidal flat dynamic action and ususally developed fluid mud on the lower tidal flat. The channel mouth deposition is the deposition in the channel mouth area. According to the sediment types, it includes sand deposition where there are coarse sediments supply and silt deposition where there are only fine sediments surpport.

峡道深水区沉积是指水深大于30米的峡道底部沉积，它以粗颗粒砂砾石沉积为特色，是现代峡道水动力对第四纪海退时发育的冲洪积和坡积物进行改造形成的蚀余沉积，全新世沉积地层往往缺失；峡道过渡带沉积是指水深介于低潮位线至30米水深线之间发育的峡道边坡沉积，该带沉积以沉积物类型多样为特色，自低潮位线至30米水深线，沉积物粒级逐渐变粗，由粉砂质粘土逐渐递变为中粗砂，是峡道深水区沉积物经多次分选沉积而发育的，基本平行于等深线分布的条带状沉积，在岸坡较陡岸段，过渡带下部可发育重力沉积；峡道潮滩沉积是指在低潮线与海岸线之间发育的细颗粒沉积，它是粘性细颗粒泥沙在潮滩动力作用下，发生动水絮凝沉积而形成的粉砂质粘土沉积，在低潮滩可发育浮泥；峡道口门区沉积则是在峡道汇入大海或海湾时，在峡道出口水流影响所及范围的沉积，根据峡道口门区供给泥沙的特性，峡道口门区沉积有粉砂质淤泥沉积和砂质沉积两种类型。

It's a good choice for very hard materials such as stone, marble and decorative edges.

这对非常坚硬材料一个很好的选择，如石，大理石和装饰边。

Jinling Chai Lin daiyu, the past, a great stone edge for Jiang strains, red pearl grass will god of nepheline palace, the waiter will dew to the earth also do with tears.

1金陵十二钗之首，前世为三生石边的一株绛珠草，受赤霞宫神瑛侍者的甘露之惠，愿跟其下凡还尽眼泪。

Study on the lithology and petrology (fine-grained cold-quenching ring of the enclaves, the reverse vein, the complex enclaves, the plagioclase phenocryst from both host rock and enclaves that is consist on the crystal form, composition and light, et al.), petrogeochemistry (Y/Nb=2.77～6.82, La/Nb=0.91～4.33, Ba/Nb=0.13～37.86, et al.), Sr and Nd isotope most ISr between 0.7031～0.7041,εNd(t=5.2～7.1 and LA-ICP-MS zircon U-Pb dating (the host rock age is 311±12Ma, and enclaves is 306±7Ma), believe the Huangyangshan pluton is crust-mantle hybrid genesis.

通过岩石学和岩相学（包体细粒淬冷边，反向脉，复合包体以及寄主岩石和包体中斜长石斑晶在形态、成分、光性上的一致性等），岩石地球化学（Y/Nb=2.77～6.82，La/Nb=0.91～4.33，Ba/Nb=0.13～37.86等），Sr和Nd同位素（ISr多数在0.7031～0.7041，εNd在5.2～7.1之间）以及LA-ICP-MS锆石U-Pb测年（寄主岩石为311±12Ma，包体为306±7Ma）综合研究认为黄羊山花岗岩是壳-幔源岩浆混合成因的。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。