滑褶皺 的英文怎麼說

中文拼音 [gǔxízhòu]
滑褶皺 英文
gleitbrett fold
  • 滑 : Ⅰ形容詞1 （光滑; 滑溜） slippery; smooth 2 （油滑; 狡詐） cunning; crafty; slippery Ⅱ動詞（貼著物...
  • 褶 : 名詞（褶子） pleat; crease; fold; wrinkle
  • 皺 : Ⅰ名詞（皺文） crease; wrinkle; crinkle Ⅱ動詞（起皺紋） wrinkle up; crumple; crinkle; crease
  1. This paper studys basement fold, capping fold, arc structure and magma activity in xingguo area, preseats the concept. of spinning - decollement structure in the area, and makes inquisiton of its mechaninsm of formation

    摘要通過興國地區基底褶皺、蓋層褶皺、弧形構造及巖漿活動的研究，闡述了該區旋滑構造的特徵，並對其形成機制進行了探討。
  2. Sliding structures are recognized appling multiple ways, and they occur in sections in the shape of flowers. the main sliding fault has the characteristics of straightness and sectionality in plane view. in the main displacement belt or its adjacent areas, an echelon faults and an echelon folds appeared

    應用多種標志識別走滑構造，主要表現為剖面上出現花狀構造，主走滑斷層平面上呈平直狀和分段性，在主位移帶內或其毗鄰地區出現雁列斷層及雁列褶皺，在主幹斷裂帶兩側的褶皺構造可見火山巖體被錯開，位移2 4km ，在鉆井巖心樣品中見到明顯的走滑構造運動形跡。
  3. Thermal deposits mainly formed during middle - late yanshanian age, related to extension structure, with main mineralization in qingfeng competent deformation zone, western shennongjia fault arch, northern huangling fault arch, xianfeng anticline of enshi platforman fold bundle

    熱液型鉛鋅礦床主要形成燕山中晚期，與滑脫拆離構造密切相關，礦化主要集中於青峰強變形帶、神農架斷穹西部、黃陵斷穹北部、恩施褶皺束咸豐背斜、長陽褶皺束走馬坪背斜中。
  4. According to the spread of nappe and relation between the nappe and depression, oblique - thrust fault zone was divided into three parts in this paper : sertengshan, lvliangshan and xitieshan. ( 3 ) according to macroscopic characteristics of fault zone, cleavage characters of fault zone, drag folds, the reverse " s " fold in the footwall, positive flower structures and small left strike - slip fault, the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section, left - slip fault in plane and the strike - slip displacement increasing from the west to the east

    （ 3 ）根據斷裂斷裂帶的宏觀特徵、斷層帶劈理特徵、斷裂帶附近的牽引褶皺和斷層下盤的平面反「 s 」型褶皺以及斷層上盤剖面正花狀構造和平面左行小型平移斷層，認為賽什騰-錫鐵山斷裂帶運動學主要表現為剖面上的逆沖、平面上的左行走滑特點，並且走滑量具有自西向東增大之勢。
  5. The first phase involves the formation of thrusting and napping towards nww accompanied by extensive igneous activity and mineralization. the second phase corresponds to the development of asymmetrical small fold downwards north and south. the final phase the cenozoic is marked by strong brittle fractures activity resulting in the sharp heave of the landform of xiaoqinling aera

    太華群內的褶皺及南北兩側斷裂分析表明，小秦嶺燕山期至少經歷3期變形，第一期為sse nww向的褶皺變形作用；第2期為南北向正斷下滑剪切作用；第3期為脆性正斷作用。
  6. 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。
  7. 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

    通過對鄂爾多斯盆地西緣構造發育的區域構造背景分析，認為在鄂爾多斯盆地之西，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拉善地塊，受南北相鄰的祁連褶皺帶和天山興蒙褶皺帶活動的影響，較穩定地塊的范圍比較狹窄，其南又有龍首山-中衛走滑斷裂構造帶存在。
  8. Bend - glide folding

    曲滑褶皺
  9. Flexural - slip fold

    曲滑褶皺
  10. 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。
  11. This collection of designs uses high - grade linen uniquely knitted to enhance crease - resistance, thus distinguishing it from traditional flat - woven material. blended of smooth viscose rayon, the fabric possesses a soft, delicate, romantic touch, allowing the skin to breathe freely, and its cozy, carefree feel brings comfort to both body and soul

    突破一般亞麻平織方式，採用獨特的亞麻針織法，具有不易皺褶的特性，以高級亞麻為主要素材，混以觸感柔順光滑的人造絲viscose rayon ，將亞麻從未展現的溫柔細致與浪漫呈現出來。
  12. The main research progresses of this thesis are shown as follow : 1. the a - c films with notably different surface micro - morphology were successfully fabricated by adjusting the sputtering process. there features change from smooth to a fractal - like structure with abounding holes and complicated gofers

    本論文的主要的研究工作進展如下: 1 .通過調控濺射工藝成功制備具有顯著差異的表面形貌的非晶碳薄膜，其表面特徵為從光滑平坦過渡到具有豐富的孔隙和極其復雜的皺褶的分形結構。
  13. The main fabric is linen, " the queen of yarns, " which is highly efficient in absorbing moisture and dispersing heat, and is also resistant to decay and bacterial build - up. the fabric is of a knit construction and its linen yarn is mixed with viscose rayon, providing a soft, smooth texture. this new series of men s fashions is also highly ventilating and crease - resistant

    Sm天衣新近推出新浪漫亞麻夏日男裝系列，採用具有良好吸濕散熱防腐和抗菌等功能的紡織原料皇后亞麻為主要素材，混以觸感柔順光滑的人造絲viscose rayon ，並特別採用針織方式，使這系列男裝更展現出透氣涼爽不易皺褶的特性。
  14. With the field work and plenty of references, the influence to the generation and development of the deformed slopes in badong formation is discussed in this paper

    造成三峽庫區發育深厚層鬆散斜坡的構造主要包括褶皺、多層次的順層滑脫構造、強烈發育的劈理等。
  15. Analyzing collected dada, the conclusion is : northwestern trending right lateral strike slip faults are predominant, other active structures include northeastern trending left lateral strike slip faults and west - east trending folds

    對上述資料分析認為：天山山間主要以北西向的右行走滑活動斷裂為主，另有一些北東向的左行走滑活動斷裂和東西向的活動褶皺。
  16. This paper studys basement fold, capping fold, arc structure and magma activity in xingguo area, preseatsthe concept. of spinning - decollernent structure in the area, and makes inquisiton of its mechaninsm of formation

    通過興國地區基底褶皺、蓋層褶皺、弧形構造及巖漿活動的研究，闡述了該區旋滑構造的特徵，並對其形成機制進行了探討。
  17. Viscose staple fiber with high moisture is a kind of cellulosic fiber with relatively higher dry - strengh and wet - strength ， and wet modulus, whose material is high quality cotton and wood pulp being 100 natural regenerated fiber, it has a soft and lubricious feeling, and a strong feeling of silk touching it will give you a very comfortable feeling

    高濕模量粘膠短纖維是一種具有較高的干強、濕強度、濕模量的纖維素纖維，它是以優質棉木漿為原料的100的天然再生纖維，纖維質地柔軟滑爽，絲質感強，具有良好的手感和懸垂感，織物形態穩定性強，耐洗滌，抗褶皺，穿著舒適。
  18. Situated at the both e w sides of pamir, the s w tarim and tadjik basins have the similar evolution history of tectono sedimentary processes during cenozoic, i. e. steady subsidence with transgressive sequence in paleogene and speedy subsidence with continental molassetype sediments in strong compressive tectonic environment in neogene - quaternery. since neogene, for the effect of pamir and west kunlun s northward moving and thrusting, there is complicated tectonostructural deformation taking place in tadjik and sw tarim. neogene stratigraphic combination and later structural deformation of tadjik basin and southwestern tarim much resemble each other in terms of extent of transpressional processes. paleogene in tadjik basin is main oil - bearing sequence and many substantial oil - gas fields there have been found. so, it can be assured in comparison that there is oil - gas perspective also in southwestern tarim region

    第四紀受強烈擠壓快速沉降接受陸相磨拉石沉積。自新第三紀以來，受帕米爾西昆侖北移和隆升沖斷的影響，塔西南和塔吉克盆地發生了復雜的褶皺沖斷變形，其差異在於塔西南明顯地受走滑為主的剪壓構造作用，而塔吉克盆地是受擠壓為主的剪壓構造作用的影響。塔西南和塔吉克盆地下第三系巖相組合類似，後期構造變形也相似，塔吉克盆地下第三系是該盆地的主力油層，已有許多油氣田發現，因此可以推斷塔西南也應該有良好的油氣前景。
  19. Compared with average filter method, the method can eliminate the noise information in the measurement points more effectively. a data compression method was proposed to compress the measurement points that include huge redundancy under certain accuracy. then segmentation and smoothing method for the measurement points to identify the jump edge, crease edge and smooth edge and optimize the measurement points were conducted so as to reconstruct the surface and generate the manufacturing path conveniently

    在一定的精度條件下，該方法可對包含大量冗餘的測量數據進行壓縮處理；對測量數據進行分片處理，拾取測量數據中的階躍邊界點、褶皺邊界點和光滑邊界點並優化測點數據，從而便於對測量數據進行nurbs （ non - uniformrationalb - spline ）重建和加工路徑生成等后續處理。
  20. A right lateral strike slip, which is shown by mapview distribution of the whole fault zone, displacement of the strata, drag folding, s - c fabric and association of subsidiary faults, forms the mainly deformational mechanism

    右行走滑活動的主要標志包括斷裂帶的平面展布、地層錯動、牽引褶皺、 s - c組構、次級破裂組合等。
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