sea crust 中文意思是什麼
sea crust
解釋
船體水下部分附生物-
Amore 2001 has successfully investigated the gakkel ridge and arctic ocean in vicinity of its geological and geophysical nature, as well as the nature of sea ice and biology in this area. the preliminary onboard petrology and bathymetry results show that the mantle beneath the gakkel ridge with low temperature has only encountered very low degree partial melting during the spreading and there is no any direct relationship between the crust nature and the spreading rate along the gakkel ridge in any simple petrologic way. mantle temperature and fracture zone density also play a major role on the crust nature, besides spreading rate
對所取得資料的初步研究表明gakkel洋中脊之下的地幔僅經受了較低程度的部分熔融，具有較低的溫度。 gakkel洋中脊處的地殼性質和巖漿活動與擴張速率之間不存在任何直接的巖石學相關性，擴張而導致的巖石圈頂部的冷卻並不是決定洋脊處地殼性質的最重要因素。地幔溫度和斷裂帶的存在與否及其密度對地殼性質具有重要的影響意義。 -
The outer hard crust of earth is made up of a dozen or so hard plates that drift on extremely hot, soft rock like floating islands on a sea
地球外部的堅硬外殼由大約12個板塊構成。就像在海上漂流的島嶼一樣，這些板塊在極端高溫的地下巖漿上漂移。 -
To strip it from sea - bed rock and transport it to seabank, it is necessary for us to understend the friability of cobalt crust
欲將結殼從海底基巖上剝離並采出海面，必要弄清鈷結殼的破碎特性。 -
The crust under ocean deeps would be thinner than under land surfaces at or near sea level.
深海下面的地殼比海平面或者接近海平面的陸地下面要薄。 -
Sea salt not only dissolves from rocks, it also reacts with the rocks of the ocean crust and volcanic lava. the reactions take some of the salts in seawater away from the sea
巖石溶解產生海鹽，而同時，海鹽又與大洋地殼中的巖石和火山熔巖進行化學反應，從而把一部分鹽分從海水中帶走。 -
Could this indicate the presence of an exit vent for sea water that had circulated through the earth's crust ?
莫非這表明存在一個環流地殼的海水出口么？ -
Explorative study on short - range exploration method for deep - sea cobalt crust tiny terrain
一種深海鈷結殼微地形近程探測方法的探索研究 -
According to the topography and geomorphology, the abnormality of gravitation and magnetic field, characteristics of crust structure and the environment of lithospheric dynamics in the northwestern of the south china sea, the seismic profiles were explained across the yinggehai basin and xisha trough
摘要本文根據南海西北部殼體的地形地貌、重磁場異常和地殼結構特徵和巖石圈動力學環境，對穿過鶯歌海盆地和西沙海槽的地震剖面進行解釋。 -
On the other hand, the coastal system ' s natural adaptive response ( resilience and resistance ) to sea - level rise would induce or increase the potential risk. the changes of the coastal risk to sea - level rise are related to the coastal environment ( geology, geomorphology, coastal height, coastal slope and local ascend and subsidence trend ). the coasts with high elevation, steep coastal slope, rocky cliff, and ascending stabilization are considered to be of higher autonomous adaptive capacity, and the lower autonomous adaptive capacity areas generally occur at lower - lying beach areas and delta coasts where coastal slope is low and the crust is descending
另一方面，海岸帶對海平面變化的自然適應能力（ 「彈力」和「阻力」 ）將使其對海平面變化的「敏感性」減少或增大，海岸自然適應能力與海岸帶的海岸環境（地質、地貌、海岸高程、海岸坡度，地殼升降運動等）有關，海拔高、海岸坡度大、地殼長期穩定上升的基巖海岸的自然適應能力較強，反之，海岸坡度平緩、地殼長期下降、地勢平坦的平原海岸和三角洲海岸的自然適應能力較弱。 -
Abstract : sea - floor cobalt crust is rich in such metals as mn, co and ni, and has been one of recently - exploited and investigeted mineral resources
文摘:海底鈷結殼富含錳、鈷和鎳等金屬，是人類近期勘探和開采研究的熱點之一。
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