陸緣海 的英文怎麼說
中文拼音 [liùyuánhǎi]
陸緣海
英文
continental margin-sea-
This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible
按照不同構造層,研究了各構造層的構造特徵:基底構造層:受早海西期構造作用的影響,與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關,為一構造變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層:受中海西區域性伸展斷陷作用的影響,盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合,如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。Geotectonically, the youjiang sedimentary basin was referred as youjiang yindosinian folded belt. triassic turbidites accumulated in the basin were derived from surrounding ancient lands including yuebei, jiangnan, and yunkai. tectonic setting of the sedimentary basin was in between an active continental margin and a continental island arc
賦礦濁積巖系的主要物源區為盆地周圍的「越北古陸」 、 「江南古陸」和東邊地區包括欽防海西褶皺帶在內的「雲開古陸」 ,沉積構造背景介於大陸島弧和活動大陸邊緣之間的過渡構造環境。The landd welling ancestors of this modern king of the sea were hunters with legs and the jaws and teeth of killers. their favorite hunting grounds were probably shallow waters near the mouths of rivers or off a level stretch of coast, for fish, both finny and shell, were then more plentiful and easier to catch than animals. because of this, these land mammals came to spend more and more time in the water
這個現代海中之王的陸上祖先,是有腿有顎有利齒的獵手。它們最喜歡的狩獵場,是靠近河口或是平坦海岸的近海淺水區,因為當時有鰭的魚類和貝殼類動物比現在要多,而且比其它動物更容易捕捉。由於這一緣故,這些陸地上的哺乳動物便逐漸在水中呆得越來越長了。The author also suggested that the fuxin block developed on the base of the geosyncline in the huabei craton, and had experienced three period process of orogeny, including hercynian folding orogeny in continental margin, mainly indo - sinian to early yanshanian intracontinental fold - faulting orogeny, and late yanshanian to early himalayaian intracontinental range - basin post orogeny
認為阜新地塊是在克拉通裂陷槽基礎上發育起來的,經歷了海西期陸緣褶皺始造山、印支?早燕山陸內褶斷主造山、晚燕山?早喜馬拉雅陸內盆山後(重)造山等過程。All of interior greenland is covered by ice, leaving only a narrow fringe of land along the coast.
所有格陵蘭的內陸都被冰覆蓋著,只留下沿海一條狹窄的陸地邊緣The recent history of korean peninsula is a history of convergence of sea power and land power, which is an inevitable result caused by its geographical politics. during the recent history, great powers around once attempted to divide the buffer region - - korean peninsula time and again. during the cold war, the political division of korean peninsula is actually a reality of aspirations
韓半島的近代史是一部成為海洋勢力與大陸勢力之力量交匯處的歷史,這是其地緣政治意義所導致的必然的結果。在近代的歷史上,周邊列強曾多次試圖分割東亞的緩沖地帶- -韓半島。冷戰時期,韓半島政治上的分裂實際上就是這種慾望的實現。If all goes well, the hybrid rov will let scientists better understand fundamental processes occurring at the deep subduction zones along the continental margins where geochemical recycling of the earth ' s crust takes place
如果一切都進行得很順利,復合型遙控探測器將可使科學家更清楚地了解,發生在大陸邊緣海洋深處隱沒帶的地質變化,以及此處地殼物質所進行的地球化學循環內容。Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences. the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )
通過研究有以下成果及認識:鄂爾多斯盆地及其周緣地區沉積蓋層可劃分為五大構造層序,盆地的形成和演化分為六大構造階段:太古代至古元古代基底形成階段、中新元古代克拉通內裂陷槽或坳拉槽演化階段、震旦紀?早古生代華北陸表海盆演化階段、晚古生代?早中生代華北克拉通坳陷演化階段、中生代中晚期大鄂爾多斯內陸盆地演化階段及獨立鄂爾多斯盆地的形成、新生代周緣斷陷盆地演化階段。The sedimentary formation can be summarized as rift bay filling sequence, epicontinental sea filling sequence, offshore debris lake basin sequence and inner continental lake basin sequence. a framework of sequence stratigraphy for the upper palaeozic strata is established in the area. the helan aulacogen of upper carboniferous in the west margin of ordos can be divided into 12 sequences, and most of the upper palaeozoic strata in the area can be divided into 15 sequences
本文對研究區內上古生界進行了層序地層學探討,將本區沉積建造概括為裂陷海灣充填層序、陸表海充填層序、近岸碎屑湖盆層序和內陸湖盆層序,建立了研究區上古生界層序地層學格架,西緣賀蘭拗拉槽上石炭統劃分為12個層序,本區大部分地區上古生界可劃分出15個層序,並全面地概括了層序演化各階段的具體特徵。These characteristics make it very clear that factors influencing the sea - atmospheric exchange of co2 in marginal continental shelf seas are very much complicated than those in open oceans
上述分佈特徵表明,陸架邊緣海海一氣二氧化碳交換的影響因素較大洋要復雜得多。So it had the long distance controlling effect on the sediment in the ordos. it is generally supposed that on the ramp of cratonic basin, the sequence of the epicontinental sea in the ordos is mainly composed of the transgressive system tract and the high stand system tract. this paper shows that it is possible that the incised valley of the low stand system tract can exist on the continental shelf in the basin
鄂爾多斯地區上古生界具有克拉通盆地陸表海緩坡沉積的一般特徵,層序構成一般以海侵和高位體系域為主,本次研究認為在陸表海沉積背景下,除在大陸邊緣附近,在盆地內古大陸架上也可以發育低位體系域的下切河谷充填沉積。Sedimentary evolution underwent three stages included in the evaporation sea bay of the earlier stage, shallow sea basin of the middle stage, extensive sea of the continental margin
沉積演化經歷了早期蒸發性海灣、中期淺海盆地、晚期陸緣廣海的過程。Under the tectonic backgrounds of island arc belt, fore - arc trench belt, back - arc basin, and epicontinental active belt of late paleozoic, it has different volcanic rock characteristics
在晚古生代島弧帶、弧前海溝帶、弧后盆地或陸緣活動帶等構造環境下發育有不同的火山巖組合。Based on development platform and the software designing, we develop a self - governed and perfect database system for surface wave tomography in china and its adjacent land and sea areas. this database system is helpful and important for probing into the deep earth, the form and evolvement of lithosphere / asthenosphere, the form and evolvement and the relation of surface structure and deep structure of chinese continent
為對這些海量數據進行合理有效管理,作者採用發展較成熟的開發平臺和軟體設計方法,開發一個獨立、功能完善的「中國及相鄰陸域海域面波層析成像數據庫系統」 ,對研究地球深部過程,對了解中國及鄰區邊緣海巖石圈軟流圈形成及演化,了解中國大陸形成及演化以及地表構造與深部結構的關系都具有極大幫助和重要的意義。Of this total, approximately 360 million square kilometers, or 71 percent, are represented by the oceans and marginal seas
其中大約三億六千萬平方公里,即地球總面積的71 % ,為各大海洋和陸緣海。Nantian yizhu the pillar of southern heaven is located in tianya haijiao end of sky and the corner of the sea scenery district, located at southwest seaside of sanya city, hainan island
南天一柱位於海南島三亞市西南的天涯海角風景區。其總體規劃陸地面積10 . 4平方公里,海域面積6平方公里,僅次於三亞市西南海濱,意寓為天之邊緣,海之盡頭。Nantian yizhu ( the pillar of southern heaven ) is located in tianya haijiao ( end of sky and the corner of the sea ) scenery district, located at southwest seaside of sanya city, hainan island
南天一柱位於海南島三亞市西南的天涯海角風景區。其總體規劃陸地面積10 . 4平方公里,海域面積6平方公里,僅次於三亞市西南海濱,意寓為天之邊緣,海之盡頭。In the northeast continental shelf in ecs, the kuroshio intruded towards north in several branches in winter, while in summer, the kuroshio intruded the northern shelf through continental marginal flow
東海東北部陸架海域冬季黑潮以其分支形式向北入侵,夏季則主要以大陸邊緣流的形式向北進入陸架。Is a marginal sea, largely surrounded by land, and possesses some characteristics of coastal and open sea
南海是一個被陸地所環繞的邊緣海,具有近海和大洋的某些特性。In the study of global carbon cycle, the continental margin, being considered one of the potential sinks of the missing term of carbon, has become the focus of researches in the past few decades
針對目前全球碳循環中的循環途徑不閉合的問題,大陸邊緣海因被認為是碳循環中丟失項( missingterm )的可能去處,而成為研究的焦點。分享友人