片语

oceanic crust type大洋壳型

pristine oceanic crust古洋壳

oceanic c crust海洋地壳

remainder oceanic crust残余洋壳

oceanic crust belt洋壳带

oceanic crust research大洋地壳研究

oceanic cobalt crust富钴结壳

paleo-oceanic crust古洋壳

oceanic crust subduction洋壳俯沖

英汉例句

• inthis article, the relationship of odp with the research of oceanic crust is discussed.

  本文论及了odp与大洋地壳研究的关系。

• continental crust averages some 25 miles (40 kilometers) thick, although it can be thinner or thicker in some areas. oceanic crust is usually only about 5 miles (8 kilometers) thick.

  大陆地壳平均厚度25英里（40公里），虽然在某些区域会稍厚或稍薄。

• both oceanic crust and continental crust type volcanic actions influenced the forming of the great ice age.

  洋壳型火山与陆壳型火山共同作用形成大冰期。

• the oceanic crust thus serves as a magnetic tape recording of the history of the geomagnetic field that can be dated independently;

  这样海洋壳就扮演了磁带的角色，记录下可以鑒定时 间的地磁场的历史。

• in subduction zones, where older and colder oceanic crust descends beneath another tectonic plate, deep focus earthquakes may occur at much greater depths (up to seven hundred kilometers).

  在隐没带，当更老的和更冷的海洋地壳下降到另一个构造板块下面时，深震源地震可能会发生在非常深的深度（达到700公里）。

• yellow sea area, located between the margin of china「s mainland and the oceanic crust of the western pacific ocean, has transitional crustal structure.

  中国大陆边缘和西太平洋洋壳之间的黄海海域，属于过渡型地壳结构。

• degassing impulses give rise to the strengthening of oceanic crust spreading which is correlated with phases of diastrophism creating folded orogenic belts.

  排氢脉沖导致洋壳扩张的增强，而此则与创造出造山带的地壳变动幕相关。

• some archean greenstone belts represent collages of allochthonous fragments, among which oceanic crust slices are identified with characteristics distinct from the phanerozoic ophiolites.

  部分太古宙绿巖带由不同的构造单元拼合而成，并发育不同于显生宙蛇绿巖的大洋壳巖石组合。

• by 2011 scientists aboard a japanese deep-sea drilling ship called chikyu hope to start drilling through a thin piece of oceanic crust to reach earth」s mantle.

  2011年，科学家们将登上日本一艘名为「地球号」的深海鉆井船，他们希望通过鉆开一块薄的大洋地壳到达地幔。

• both subducted continental and ancient tethyan oceanic crust contributed to enriched mantle source region.

  巖浆形成于大陆弧的构造背景，俯沖的陆壳和古特提斯洋壳对富集的源区均有贡献。

• the existence of recycled basaltic oceanic crust in the axial zone of mantle plume may be the key of the formation of giant v-ti-magnetite deposits.

  巖浆源区再循环玄武质洋壳的存在可能是该区超大型钒钛磁铁矿床形成的根本原因。