褶間的 的英文怎麼說
中文拼音 [xíjiānde]
褶間的
英文
interplical-
The core of the anticlinal fold, which is squeezed between faults, underwent intense crushing.
背斜褶皺的核部在斷層間受到擠壓,遭受到很強的破壞。The shapes of ascospore for 101 # bred hybrid new specie is between the shapes of its parents by breeding the inoculated hypha from flammulina velutipes and qude mansiella radicata
通過金針菇與茶菇的菌絲融合培養,培育的雜交新品種101 #在形態及菌褶中孢子和囊體的形態上介於兩親本之間。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。Folds of scarlet drapery shut in my view to the right hand ; to the left were the clear panes of glass, protecting, but not separating me from the drear november day
在我右側,緋紅色窗幔的皺褶檔住了我的視線;左側,明亮的玻璃窗庇護著我,使我既免受十一月陰沉天氣的侵害,又不與外面的世界隔絕,在翻書的間隙,我抬頭細看冬日下午的景色。The studied deposit area is located on a monocline geotectonic unit divided by several groups of faults. therefore, the secondary widen transverse and lognitudinal drapes may have great influence on ore forming and location
礦區基本構造為一個被幾組斷裂破壞的單斜構造,其上發育的次一級的開闊型橫向和縱向褶皺對礦床的形成和空間定位起著十分重要的作用。He wore a long unsleeved garment of recently flayed oxhide reaching to the knees in a loose kilt and this was bound about his middle by a girdle of plaited straw and rushes
他身穿用新近剝下來的公牛皮做的坎肩,長及膝蓋,下擺是寬松的蘇格蘭式百褶短裙。腰間系著用麥稈和燈心草編織的帶子。Effective value of pleats in folk costume
民間裙裝中褶皺的效用價值The basin - formed mechanism, evolution model and petroliferous geological features of compresso - shear basins in the world are analyzed, by which six aspects of the features are summarized as follows : 1 ) in the compresso - shear process, the sedimentary speed of basin is high, forming thicker coarse - grained clastic rocks which normally shape good petroleum reservoir ; 2 ) the source rocks of basin tend to coming from the organic matter - enriched rocks formed in pre - compresso - shear stages, except that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in pre - compresso - shear stages, e4xcept that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in frontal of deep depression ( fore deep ) of thrust belt ; 3 ) the en echelon folds ( including anticline and fault - nose structure ) are generally as good oil traps ; 4 ) the compresso - shear process is helpful to hydrocarbon accumulation ; 5 ) it may promote the maturity and hydrocarbon - generating process of organic matte, and 6 ) the thrust belts in the surrounding areas of compresso - shear basin are favorable are favorable domains for petroleum concentration
摘要通過對世界上壓扭性盆地的成盆機制、演化模式和油氣地質特點分析,總結壓扭性盆地具有6個方面的石油地質特徵:壓扭作用期間盆地的沉積速率較高,一般形成較厚的粗碎屑沉積,它們常構成很好的油氣儲集層:盆地的烴源巖往住來自於前壓扭期砂成的富含有機質的巖石,但在強烈的壓扭作用期間,在沖斷帶的前緣深坳陷(前淵)中有可能發育深水半深水相的烴源巖;壓扭(張扭)作用期間形成的雁行式褶皺(包括背斜和斷鼻等)往住是很好的油氣圈閉;壓扭作用易於成藏;壓扭作用可以促進有機質的成熟生烴作用;壓扭性盆地的周邊沖斷帶是油氣賦存的有利部位。Growth strata and their application in timing deformation of foreland thrust - fold belts in the north margin of tianshan
生長地層及其在判斷天山北緣前陸沖斷褶皺帶形成時間上的應用The cbm industrial production region lies in transition zone which is one part of a single continent in u. s. a., but a compound continent that is made up of some small platform, landmass and fold belt in china
我國是一些小型地臺、地塊及其間的褶皺帶鑲嵌起來的復合大陸,煤層氣勘探有利區位於地臺內部。The reservoir is located at yishan slope area between jinxi fold belt and tianhuan depression, it has the characters of less structural deformation, overlying hydrocarbon genetic center in upper and lower palaeozoic era, growth of high efficient reservoirs and as well as fast lateral changes of reservoir physical properties, it has the condition of forming non structural traps, which is the major area for gas reservoir exploration in the basin
位於晉西撓褶帶和天環坳陷間的伊陜斜坡區,因具有構造變形微弱,上、下古生界生烴中心疊置,高效儲層發育,儲集層物性側向變化快等特點,具備形成非構造圈閉優越條件,為盆地氣藏勘探約重點區帶。Yanqi basin is an intermont basin of tian shan, there is a nww trending right lateral strike slip active fault in southwestern basin, its maximum slip distance is 210m, and slip rate is about 10mm / yr, moreover, there is a west - east trending active anticline along northern basin
焉耆盆地是一個天山山間盆地,盆地西南緣發育一條走向北西西的右行走滑活動斷層,最大走滑距離為210m ,走滑速率約10mm / yr ,盆地西北緣發育走向近東西的活動褶皺。Folds of scarlet drapery shut in my view to the right hand ; to the left were the clear panes of glass, protecting, but not separating me from the drear november day. at intervals, while turning over the leaves of my book, i studied the aspect of that winter afternoon
在我右側,緋紅色窗幔的皺褶檔住了我的視線左側,明亮的玻璃窗庇護著我,使我既免受十一月陰沉天氣的侵害,又不與外面的世界隔絕,在翻書的間隙,我抬頭細看冬日下午的景色。The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic
盆地基底由前寒武紀結晶基底和古生代褶皺基底組成,盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖;中二疊統蘆草溝組的暗色泥巖、泥灰巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖;三疊系雜色砂礫巖、砂巖及灰色泥巖(下紅上灰) ;以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。This paper discusses the formation algorithm of a terrane with folds. to form a fold with less lean, triangulation from scattered points in space and surface reconstruction are used. to form a fold that has superposition along z - axis, the single - value surfaces that compose the fold should be constructed separately and assembled later
研究了帶有褶曲的巖層面的構造方法,對于傾角不大的褶曲用先進行空間三角剖分,然後重建曲面的方法構造;對于在z方向上有重疊的褶曲先構造出各單值曲面然後組合起來得到。The dislocation interfaces of early stage were controlled by the slide of the ne fold. the dominant dislocation interfaces, in the dam area, is the one of the second stage, which resulted from the slide of the lava layer and lagerkluftes from nw to se because of the affect of the majiaheba faultage ' s thrusting overriding to the dam area from nw to se. the dislocation interfaces of the third stage were the result of the overprint of the structure of ne to the one of nw
早期階段形成的錯動帶受控于北東向縱彎褶皺的層間彎滑機制;第二階段形成的錯動帶在壩區佔主導地位,它們是由於北東向馬家河壩斷層由北西向南東的滑脫逆沖推覆影響壩區,並造成壩區向南東緩傾的巖層沿原生構造面向南東滑動的結果;第三階段形成的錯動帶則是由於北西向構造疊加於早期北東向構造之上而致。To sum up the above analysis, we make sure that the pretertiary of haijiao uplift, yushan uplift and east flank in oujiang depression and the transitional zone between changjiang depression and xihu depression is a new prospect of time and space for hydrocarbon exploration in the shelf basin of the east china sea
因此,海礁凸起、漁山凸起、甌江凹陷東側、長江凹陷與西湖凹陷之間以及浙閩隆褶帶的前第三系是東海陸架區油氣勘探的新領域。Now that martin was aroused in such matters, he swiftly noted the difference between the baggy knees of the trousers worn by the working class and the straight line from knee to foot of those worn by the men above the working class
既然這類事已引起注意,他很快便發現工人階級膝蓋鬆弛的褲子跟地位較高的人從膝蓋到腳背有一條筆直的褶痕的褲子之間的差異,而且找出了原因。The common affected areas are finger webs and the skin folds of wrists, armpits, buttocks, groins, elbows, nipples and lower abdomen
受影響范圍為手指間的皮膚,以及手腕腋窩臀部腹股溝肘部乳頭及下腹等部位的皮膚褶。The south africans telling their stories in these pages are from lusikisiki, a rural region in the eastern cape province, where huts cradle in the creases of green hills
這些南部非洲的居民告訴我的故事來自於魯塞濟斯基,位於東岬省的鄉間,棚屋村落從那些綠色山間的皺褶里延伸出來。分享友人