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Because of the crustal structure in the Central US which efficiently propagates seismic energy, shaking from earthquakes in this part of the country are felt at a much greater distance from the epicenters than similar size quakes in the Western US.

由于地壳结构,在美国中部有效地宣传地震能量,摇头,从地震在这部分的国家认为,在一个更大的距离震中较类似规模的地震是在美国西部。

Magnetic sus- ceptibility of these formations was obviously lower than the Archean high-graded metamorphic crystalline basements, while the responding ductile shear zones created enhanced anisotropy magnetic susceptibility attributed to their penetrative mineral lineations, both of them contributed to the crustal scale NEE-NNE striking linear aeromagnetic anomalies.

不同规模的古元古代活动带彼此并不相连,以发育变质沉积-火山岩建造为主体,岩石磁化率明显低于太古宙高级变质结晶基底,与之相关的韧性剪切带则以其透入性矿物线理产生了增强的磁化率各向异性,两者共同构建了地壳尺度北东东-北北东向线性航磁异常带。

The present configuration of the rift, which dates from the mid-Pleistocene epoch, is probably a result of a rifting process associated with thermal currents in the earth's mantle elongated depression, trough, or graben in the earth's crust, bounded on both sides by normal faults and occurring on the continents or under the oceans.

目前的断裂结构,显示来自中世纪,也许是由于断裂的过程中与热气流在地球地幔被低压延伸到地壳地堑中,位于断层的两侧正常断裂并且断裂发在陆地或者海洋。

Pies were also a common banquet item, with the crust serving primarily as a container, rather than as food itself, and it was not until the very end of the Late Middle Ages that the shortcrust pie was developed.

馅饼也是一个共同的宴会项目,服务与地壳主要是作为一个容器,而不是食物本身,但直到最后结束的中世纪晚期的shortcrust馅饼开发。

While my favorite pastry is Pate Brisee, a shortcrust pastry, that has a buttery flavor and crumbly texture, you could use your own pastry crust recipe or even a store bought pie crust.

虽然我最喜欢的糕点是八德Brisee ,一个 shortcrust糕点,具有奶油香味和易碎的纹理,你可以使用自己的糕点地壳食谱,甚至一家商店购买馅饼皮。

There is a low-density layer at middle crust in Yinggehai region. Perhaps the strike- slip of Red River Fault Zone in Yinggehai region was taken place along the layer.

同时认为莺歌海地区的中地壳中有一低密度层存在,推测红河断裂带在莺歌海地区的走滑,很有可能就是沿着这一层发生的。

The boundary condition that the surface of the crust is kept at a constant temperature of 25℃, leads to relatively less obvious variation of temperature in the underground no deeper than 2 kilometers, so that the calculated strain rate is less than 10〓(normal geological strain rate is 10〓~10〓).

由于地表的边界效应,在深度小于2km的地壳里,温度变化相对不急剧,一般不出现大于10〓应变速率(典型的地质应变速率为10〓~10〓)。

The magnitude-8.8 quake was a type called a "megathrust," considered the most powerful earthquake on the planet. Megathrusts occur when one tectonic plate dives beneath another.

智利发生的这场里氏8.8级大地震属于&大逆冲型地震&,只有当一个地壳板块俯冲至另一板块的下方时才会发生,被认为是地球上威力最强的地震。

Wind, precipitation, temperature, and barometric pressure changes affect only the surface and shallow subsurface of the Earth.

地震发生于天气不可能影响到的地壳深层,造成地震的能量也远远超过气候变化所需的能量。

Oceanographers call tsunamis seismic seawaves because they are usually caused by a sudden rise or fall of part of the earth's crust under or near the ocean.

海洋学家称那种地震引发的海浪为海啸,因为海啸通常是由洋底或接近洋底的地壳升降所引发的。

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