岩床

单个岩床的厚度在1－200m之间，较厚的岩床有明显的结晶分异作用。

The thickness of sill varies from 1m to 200m .

在靠近岩床10m范围内，镜质体反射率（Ro）值比正常地温场条件下升高1至数倍，最高可达3.44%。

The R_0 value within 10m around the sill is 1 to several times of that at normal geothermal field condition , and can even be as high as 3.44 % .

土层中位于B层之下岩床之上的一层；由风化的岩石组成。

Beneath the B-horizon and above the bedrock ; consisting of weathered rock .

远离岩床烃源岩受热影响强度逐渐降低，直至50m以外趋于正常地温值。

The intensity of thermal effect 's impacts on the source rocks decrease progressively away from the sill , and tend to be normal geotemperature over 50m away form the sill .

它岩床上，它动摇我的光。

It rocks my bed ; it shakes my light .

这样两岸都会有坚实的岩床。

Then we 'd have solid bedrock on both banks .

深峡在岩床中凿人了几百米；

Deep gorges gouged hundreds of metres into the bedrock ;

位于上层土和岩床之间的一层土壤。

The layer of soil between the topsoil and bedrock .

岩体是多期形成的，呈岩筒、岩床产出。

The rock body was formed in several stages and seen as pipe and sill .

上复岩石的碎块可能破裂并成为岩床的一部分。

Chunks of the overlying rock may break off and become a part of a sill .

我们把这种高温带入岩床中。

And we take that high temperature and we bring it down into a rock bed .

那里拥有中国国内最罕见最丰富的鲁灰花岗岩岩床。

There is the most rare in China with the most abundant shandong grey granite rock bed .

氧同位素会随着大气水循环而变化，硫同位素则根据地球岩床的不同而变化，通过它们我们就能确定地理位置。

Oxygen isotopes vary with the water cycle , and sulfur with bedrock , so they 're location proxies .

它到达海洋，数百万吨的冰已经失去了岩床的支持上。

It reaches the ocean and millions of tons of ice have lost the support of their rocky bed .

在数千年的漫长光阴中水的侵蚀深入到岩床的心脏地带

Over many thousands of years , water has corrode its way deep into the heart of the bedrock itself .

目前，他们已在沙子和岩床中钻了500英尺，未发生坍塌

So far , it 's been able to bore through 500 feet of sand and bedrock with no collapses .

这些雕刻在石灰岩岩床上的迷宫被沙漠深埋，还有许多秘密等待发现。

Carved from limestone bedrock , these labyrinths protrude deep beneath the desert and have much left to be discovered .

岩床底上如有陷穴，就起到天然溜槽的作用，干扰了岩流体系，使硫化进一步堆积。

Sulfide further accumulates where depressions in the bottom of the sill interfere with the flow system and act as natural riffles .

在矿区中部和南部，岩床起了主导作用，造成煤种变化的多样性和复杂性。

In the middle and southern part of the mine area sill predominated , which resulted in complicated and varying types of coal .

煤层气开发有利区应在向斜翼部和岩墙、岩床附近变质程度高的煤区。

The exploiting area should be in the synclinal profile , dike and bed rock with the high level of the coal metamorphism .

当你看到岩床终端时你应该自问，侵入的岩浆在侵入期是如何表现它们的特征的。

When you see a termination of a sill you should ask yourself how the intruding magma behaved at the moment of intrusion .

后岩床皱襞与小脑幕缘的交点为标志点可定位滑车神经入小脑幕点。

The point of intersection of post bedrock folds and tentorial edge can be targeted the point of Trochlear nerve into the tentorial .

结果46.7%（14/30）的动眼神经在跨越后床突和（或）后岩床皱襞处存在压迹。

Results In 46.7 % of OMN there were OMN impressions where they strode over posterior clinoid processes and / or posterior petroclinoid folds .

二叠纪晚期到三叠纪断裂和下沉作用形成了大约9千米厚的第三纪沉积地层，在其中有岩床的切入。

Late Permian to Triassic rifting and subsidence resulted in the deposition of as much as9 kilometers of Triassic strata , locally injected with sills .

我们相信美国是一个国家，那的小生意者可定是很了不起的，因为他们有岩床，我们经济的支柱。

We believe that America is a country where small business owners must succeed , because they are the bedrock , backbone of our economy .

洪水冲洗掉地表附近松软的风化土，最终到达了岩床，哥伦比亚高原上坚硬的火山岩。

The waters scoured off the soft , windblown soil near the surface and eventually reached bedrock , the hardened lava of the Columbia Plateau .

当一群考古学家在巨石堆历史纪念碑附近挖出一具木乃伊时，一个潜藏在岩床下的远古机器部件也被发现了。

When a group of archaeologists dig up a human skeleton near the historical monument of STONEHENGE , an ancient piece of machinery hidden beneath the bedrock is discovered .

在矿区北部，花岗斑岩岩株对煤变质起了主导作用，侵入煤层的岩床的影响是局部的；

In the northern part of mine area , stock of granite porphyry played a dominate role in coal metamorphism , and intrusive sill in coal seam was found locally .

这一带地层，由砂岩堆积而成，受海浪长期的侵蚀和风化，在海边，形成陡直的海蚀崖及宽平的岩床。

The band formation , formed by the accumulation of sand , long-term erosion by waves and weathering in the sea , forming steep cliffs and wide flat rock bed .

琳达和她的同事说，这些纹路位于一块腐蚀的岩床上，高为2.5英寸。这些纹路可能是在液体流经碎岩和沉积矿物质时候形成的。

According to Kah and her colleagues , the veins which jut out 2.5 inches above a patch of eroded bedrock likely formed when fluids moved through cracked rock and deposited minerals .