鄂拉山 的英文怎麼說

中文拼音 [èshān]
鄂拉山 英文
ngola shan
  • : 名詞1. (湖北的別稱) another name for hubei province2. (姓氏) a surname
  • : 拉構詞成分。
  • : 名詞1 (地面形成的高聳的部分) hill; mountain 2 (形狀像山的東西) anything resembling a mountain...
  1. This paper use the ncep / ncar day - to - day reanalysis data of 500hpa high field and so on, choose ural mountain, baikal, okhotsk as the key district, the mid - high latitude of eurasia circulation courses that have long duration ( scale of time is middle, namely during 10 - 30 day ), maybe continue continuously after being intermittence of 1 - 2 days in middle, appear repeatedly is for research object, define an index " i " of the circulation pattern over mid - high latitude of eurasia. a method is proposed to identify the summer typical persistent circulation pattern at 500hpa levels over eurasia mid - high latitude. the climate characteristics of those typical persistent circulation patterns are studied

    本文利用ncep / ncar再分析逐日500hpa高度場等資料,選擇烏、貝加爾湖、霍次克海這三個地方作為關鍵區,以夏季歐亞中高緯度持續時間長(時間尺度屬于中間時間尺度,即10 ? 30天之間) 、中間可能會間歇1 、 2天然後又繼續持續、反復出現的環流過程為研究對象,定義了一個夏季歐亞中高緯流型指數,在此基礎上提出了一種對夏季歐亞中高緯500hpa典型持續流型的界定方法,研究了典型持續流型的氣候特徵,分析了流型指數的年代際變化,以及對應不同階段、不同流型的降水場、加熱場、海溫場等的主要特徵。
  2. The interdecadal characteristics of correlation pattern of interannual relationship between winter sea - ice extent of davis strait and august 500hpa height of northern hemisphere is " + - + " pattern from ural mountains to north of sea of okhotsk which is strongly negatively correlated with the august rainfall of north china before 1974, and it has not apparent correlation pattern in europe - asia continent after 1974

    1974年前,冬季戴維斯海峽海冰面積和北半球8月500hpa位勢高度場的相關系數呈一個自烏開始到霍次克海以北分佈的「 + - + 」型,該型和8月華北降水的反相關較好; 1974年後,相關在歐亞大陸地區變差,沒有明顯的相關型,冬季戴維斯海峽海冰面積和8月華北降水關系變差。
  3. A large amount of data of the latest regional geoglogy and the latest correlation data of layers and rock formation have been quoted, and a description of distribution of crystalline basement, formation, evolution as well as the distribution characteristic of the fracture belt of ordos basin have been made in this paper, and the paper also pointed out that the g - layer which lies between the base of the basin and tg reflector, is the extension of basinward of guandaokou of jixian system. the layer of changcheng system and jixian system, which had been divided before, can be correlated with the exposed huangqikou group and wangquankou group in helan mountain, and divided into qingbaikou system. so, the paper denied the viewpoint of the existence of aulacogen in hutuo period and middle proterozoic in this basin

    文中引用了大量最新的區域地質資料和最新的地層、巖系劃分對比資料,對爾多斯盆地結晶基底的巖系分佈、形成、演化以及斷裂的展布特徵進行了描繪,並指出盆地基底與tg反射層之間的g層是薊縣系官道口群向盆地的延伸,盆地中原劃分的長城系、薊縣系地層可以和賀蘭出露的黃旗口組、王全口組對比,亦劃歸青白口系,從而否定了爾多斯盆地存在滹沱期坳谷和盆地中有中元古坳谷發育階段的看法。
  4. Through the regional background analysis in which western structures developed, it suggested that there did not exist a united and steady block to the west of ordos basin. alashan block neighboring on the north of the western margin was largely influenced by the action of qilian and tianshan - xingmeng folded belt which is respectively to the south and north of alashan block, was narrow in the steady block and was limited by the longshou mountain - zhongwei strike fracture in the south area

    通過對爾多斯盆地西緣構造發育的區域構造背景分析,認為在爾多斯盆地之西,一直沒有一個統一的穩定地塊相鄰,與盆地西緣北部相鄰的阿善地塊,受南北相鄰的祁連褶皺帶和天興蒙褶皺帶活動的影響,較穩定地塊的范圍比較狹窄,其南又有龍首-中衛走滑斷裂構造帶存在。
  5. The study on the structural feature opened out by the non - seismic ( mt ) profile of xiaonangou in qinglong mountain on the west edge of ordos basin and the seismic profile across helan mountain shows that a series of thrust blocks - qinglong - luoshan - nioushou - helan mountain, were the thin - skin structure formed by the westward compression of ordos block and the dextral shear of alashan block

    通過對盆地西緣青龍南端小南溝的非地震mt剖面以及橫穿賀蘭的地震剖面揭示的構造形態研究認為,盆地西緣一系列推覆體青龍?羅?牛首以至賀蘭是由於爾多斯地塊向西推擠同時與阿善地塊的右行運動所產生的「薄皮構造」 。
  6. Through the analysis of subsidence history in the north of western ordos basin, as a result of the terranes northward accretion and the successive collision of the baykala block in the middle triassic, the qiangtang block in the late triassic, the lhasa block in the middle jurassic, the gangdese block in the cretaceous and the subduction of izanagi plate in yanshanian period, the studied region became a intracontinental foreland basin from late triassic to cretaceous

    摘要通過對爾多斯盆地西緣北段沉降史的分析可知,晚三疊世白堊紀,由於中三疊世巴顏喀地體、晚三疊世羌塘地體、中晚侏羅世薩地塊、白堊紀岡底斯地體連續向北增生、碰撞以及燕期伊佐奈岐板塊的俯沖,盆地西緣北段的響應顯示為陸內前陸盆地的特徵。
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