海底臺地 的英文怎麼說
中文拼音 [hǎidetáide]
海底臺地
英文
bodenschwelle-
She is the observatory of new shanghai. the view balcony on the 18th floor is the best place to take a birds - eye view of the scenery on either side of the huangpu river. from here, we can see that shanghai is growing every day and marching to the new century
她是新上海的眺望臺,登上18層的觀景平臺,浦江兩岸的風情盡收眼底,上海在她的眼中一天天長高、長大,一天天光彩照人,一步步地走向新世紀。Effect of submarine topography variation in shallow sea on dynamic characteristics of offshore platform
淺海海底地形變遷對海上平臺動力特性的影響The sea around northern sakhalin, in which the project ' s offshore drilling rigs stand, freezes for half the year and is home to a rare whale
該項目的海底鉆探平臺設在環繞北庫頁島的海域,這里每年有半年處于封凍期,是一種珍稀鯨類的棲息地。The heavy load ropes used in the sea, fishery and coast industries, fishing system, rescue system, offshore platform systen, the ropes for berth, anchoring, survey system for the ociasion earthquake, and cable systems
? ?在海洋,漁業和海岸工業中使用的重負荷繩索。海上打澇系統,救援系統,海洋石油平臺系統,停泊、拋錨、嵌入系泊線、海洋地震勘測、海底電纜系統。Figure 1 the director, mr c y lam, explained the propagation of tsunami waves as simulated by a numerical tsunami model when a hypothetical undersea earthquake occurred in the south china sea
圖一臺長林超英先生利用數值海嘯模式解釋一個假設在中國南海發生的海底地震所引發的海嘯波擴散情。Also, tsunamis generated by undersea earthquakes, and sea level change and climate change due to global warming are topics of common interest to soa and hko
此外,由海底地震觸發的海嘯全球變暖引致的海平面變化和氣候變化等都是海洋局和天文臺共同關注的課題。The palaeogeographic research indicate that the palaeogeographic outline of the study area recorded the evolution from a sedimentary basin in which the shallow - water carbonate platform sediments and deep - water terrigenous clastic submarine fan developed from southeast to northwest and northeast during the late triassic through a submarine sheet - like model composed of deep - water sandy turbidite and fine - grained turbidite during the early jurassic to a terrigenous clastic barrier coast during the middle and late jurassic and finally to the coal - bearing delta sediments during the late cretaceous
古地理分析表明,研究區晚三疊世古地理輪廓是一個從東南向西北和東北方向由淺水碳酸鹽臺地及深水陸層海底扇沉積共同發育的沉積盆地;早中侏羅世,演變成為一個由深水砂質濁積巖和細屑濁積巖組成的水下席狀體沉積;進入中晚侏羅世,其古地理表現為一個陸屑淺海有障壁海岸;到了晚白堊世,研究區表現為以含煤沉積為特徵的三角洲相沉積。分享友人