A pair of new inodorous halfsilk black ladies hose, a pair of new violet garters, a pair of outsize ladies drawers of india mull, cut on generous lines, redolent of opoponax, jessamine and muratti s turkish cigarettes and containing a long bright steel safety pin, folded curvilinear, a camisole of baptiste with thin lace border, an accordion underskirt of blue silk moirette, all these objects being disposed irregularly on the top of a rectangular trunk, quadruple battened, having capped corners, with multicoloured labels, initialled on its fore side in white lettering b. c. t. brian cooper tweedy
一雙嶄新沒有氣味半絲質的黑色女長筒襪,一副紫羅蘭色新襪帶,一條印度細軟薄棉布做的大號女襯褲,剪裁寬松,散發著苦樹脂素馨香水和穆拉蒂牌土耳其香煙的氣味,還別著一根鋥亮的鋼質長別針,折
疊成曲線狀。一件鑲著薄花邊的短袖麻紗襯衣,一條藍紋綢百
褶襯裙。這些衣物都胡亂放在一隻長方形箱蓋上:四邊用板條釘牢,四角是雙層的,貼著五顏六色的標簽,正面用白字寫有首字b . c . t布賴恩庫珀特威迪。
A convenient variation upon the process of superposition thus described is a mathematical operation designated as convolution.
對于上面描述的
疊加過程,有一種方便的變形,它就是稱為
褶積的一種數學運算。
Crista ( pl. cristae ) the structure formed by folding of the inner mitochondrial membrane, giving a large surface area for electron transport
嵴(嵴膜) :線粒體內膜向內室
褶疊形成的結構,可以為電子傳遞提供更大的表面積。
This sediment will then probably be formed into a folded and imbricated structure.
然後這些沉積物可能形成
褶皺和
疊瓦構造。
There are five kinds of fault - fold assemblage styles which are respectively thrust - nappe structures, imbricate thrust - propagation folds, face to face thrusts, back to back thrusts and positive flower structures
主要的斷層?
褶皺組合樣式有沖斷推覆構造、
疊瓦沖斷層?斷展
褶皺組合、對沖斷層?沖凹構造、背沖斷層?沖起構造和正花狀構造。
Yili basin is a independent unit of the yili - zhongtianshan micro plate, which is subject to the zhunger - kazakstan plate. it is a superimposed basin which formed on the basis of the folded pre - permian basement, underwent rifting and breaking in permian, depressing and uplifting and multiple deformation and reformation after permian
伊犁盆地是準噶爾?哈薩克斯坦板塊的一個次級構造單元?伊犁-中天山微板塊內的一個獨立單元,它是在前二
疊紀
褶皺基底的基礎上,於二
疊紀擴張、裂解(谷) ,經二
疊紀后的坳陷、隆升多期變形、改造而成的復合型改造盆地。
Further imbrication, folding and metasomatism of the ultrabasic rocks occurred at this time.
超基性巖的進一步
疊瓦作用,
褶曲和交代作用發生於這個時期。
According to characteristics of the seismic data from the low snr region with complex surface, this paper is started from solving the static correction problem and reasonable eliminating all kinds of disturbance in the seismic data from the low snr region with complex surface. through the whole process of seismic data processing which includes a series of processing methods that are suitable for the low snr region, namely, from the choosing of the floating base - level, the static correction in the field and indoors, the eliminating of all kinds of noise before and after stacking, the velocity analysis with high - resolution, the reasonable techniques of deconvolution before stacking and wavelet processing after stacking, to the method choosing of the high - resolution stacking and the reasonable and accurate offset imaging, a set of the complete and effective flow for processing seismic data from the low snr region with complex surface are finally formed, which can meet the need of explo
本文針對復雜地表低信噪比地區地震資料的特點,以解決復雜地表低信噪比地區地震資料靜校正問題及合理剔除各類干擾為出發點,在整個地震資料處理過程中,從浮動基準面的選取、野外及室內靜校正、
疊前
疊后各類噪音的去除、高精度速度分析、合理的
疊前反
褶積及
疊后子波處理技術、到選用高精度的
疊加技術及合理準確的偏移成像方法等一系列適合於復雜地表低信噪比地區的處理方法,最終形成一套較完整且有效的針對復雜地表低信噪比地區地震資料的處理流程。
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。
Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part, and belong to the miliangchuan schiefer
礦區所在部位屬南秦嶺造山帶中帶古生代伸展盆地
疊加印支期沖
褶帶的北部,隸屬于米糧川逆沖巖片。
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。
The state of being folded
褶子被折
疊的狀態
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 clues and techniques to improve the resolution of data processing are 1 ) removing the affection of near surface factors on data acquisition, including static correction and noise eliminating technique etc, 2 ) broadening the frequency band of pre - stack seismic data, including amplitude compensation and pre - stack deconvolution etc, 3 ) improving s / n ratio of high frequency and weak reflection signals through multiple coverage with high precision velocity analysis, residual static correction and high - order nmo, raising " dead line of high frequency reflection ", and 4 ) identifying post stack effective reflection frequency band, enhancing dominant frequency and so on
主要包括:消除近地表因素對資料採集的影響,包括靜校正和噪音壓制技術等;
疊前拓寬地震資料領帶,包括振幅補償和
疊前反
褶積技術等;藉助高精度速度分析、剩餘靜校正和高次項nmo技術,通過多次覆蓋
疊加,消除資料中隨機噪聲干擾、提高資料信噪比,尤其是高頻端反射信息的信噪比,改善高頻反射和弱反射信號信噪比,提高「高頻反射死亡線」 ;
疊後有限反射頗帶識別、抬高優勢頻率等。
Different rock mass on the remote sensing images were obtained, based on a comprehensive remote - structure analysis, a new acknowledge on the characteristics of regional structure in tonghuashan - yushugou area was acquired. it was suggested that tonghuashan - yushugou area underwent multi - phase structure movement, multi - phase, multi - orientation > multi - level deformed structure superimposed each other accompanied with complex deformation
通過遙感?構造的綜合解析,總結出從遙感圖像上辨識高壓麻粒地體、韌性剪切帶、
疊加
褶皺及不同應變帶、不同類型面理和不同巖體的圖像處理方法,並獲得榆樹溝?銅花山地區區域地質特徵的重新認識。
The direction of migration was in east and northeast. ( 3 ) this paper introduced the balanced section into the early reservoir description in the sidaogou structure for the first time, and gave a new viewpoint that the sidaogou structure was a fault - bend fold formed by two step thrust fault. the structural stress direction came from the northeast of the hami depression
首次將平衡剖面技術引入了四道溝構造早期油藏描述的構造研究之中,並首次提出四道溝構造是?至少由兩個階梯狀斷層組成的后傾雙重構造
疊加的斷層轉折
褶皺,構造應力方向應大致源於北東方向。
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。
Lithologically different rock sheets intertexturally superimposed with faults and folds of various styles. while, the southern belt is chiefly of devonian tuff, tuffaceous schist, marble relatively stable in strata and manifested by regional asymmetric fold easi - westward in axis, with well developed superimposed overthrust south - northward which controlled the whole structural framework in this area
南帶以泥盆系凝灰巖、凝灰質片巖、大理巖為主,地層相對穩定,表現為軸向東西的區域性不對稱
褶皺,廣泛分佈控制全區構造格局的南北向逆沖推覆的
疊瓦式斷裂。
In this region, the structure development can be divided into three stages : the formation of the east - west direction fold ; the overlaping of the south - north direction structures ; the later formation of the split basins
本區構造演化可分為三個階段:東西向褶皺的形成;南北向褶皺的疊加;後期裂陷盆地的形成。