Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase
查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內
的一個次級構造單元，其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成
的陸緣或島弧
褶皺帶，
具有古生代造山帶
的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖
的構造環境；燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶
的增厚陸殼開始發生伸展垮塌
的構造環境；早白堊世火山巖形成於造山期后進一步發生伸展垮塌
的區域構造環境。
Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin, northeastern yingen - ejinaqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate, tarim plate and kazakstan plate
查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內
的一個次級構造單元。其基底為古生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位
的陸緣或島弧
褶皺帶，
具有古生代造山帶
的性質。
Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous, is featured by simple sedimentary feature, depositional cycle, small lacustrine transgressive, dry climate, salinization lacustrine water and multi - and - near sources
摘要二連盆地是在海西期地槽
褶皺基底上發育起來
的早白堊世斷陷湖泊群，
具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸化、沉積旋迴單一，多物源、近物源和粗碎屑等沉積特徵，以及發育巖性地層油氣藏為主
的油氣分佈特點。
Tufted with tillers, short rhizomes and stolons ; leaf folded in bud ; leaf blade bluish green, linear with boat - shape tip ; inflorescence an open panicle ; seeds awnless. flowers from april to june
本種?簇生形，
具分? * ，亦
具短
的根莖及匍匐莖；葉在芽期是
褶生；葉片藍綠色，長條狀，前端成船狀；花序?開放圓錐花序；種子無芒；花期4至6月。
According to the fact that the basic features of apalmprint, including principal lines, wrinkles and ridges, havedifferent resolutions, in this paper we analyze palmprints using amulti - resolution method and define a novel palmprint feature, whichcalled wavelet energy feature, based on the wavelet transform. wef can reflect the wavelet energy distribution of the principal lines, wrinkles and ridges in different directions at different resolutions scales, thus it can efficiently characterize palmprints. this paperalso analyses the discriminabilities of each level wef and, according to these discriminabilities, chooses a suitable weight for each levelto compute the weighted city block distance for recognition. theexperimental results show that the order of the discriminabilities ofeach level wef, from strong to weak, is the 4th, 3rd, 5th, 2nd and 1stlevel
作為對現有人體生物特徵識別技術
的重要補充，掌紋識別有著其獨特
的優點：掌紋比指紋含有更多
的可區分信息掌紋採集設備
的價格比虹膜採集設備
的價格要低廉得多掌紋特徵比簽名特徵更為穩定掌紋識別可獲得比人臉識別更高
的識別精度掌紋含有獨特
的線特徵包括主線和皺
褶，這些線特徵
具有很強
的區分能力，並可以在低解析度圖像中提取出來可以將手掌上
的各種特徵融合在一起建立一個高精度
的生物識別系統等。
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。
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。
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。
Different tectonic style exists in the upper and lower layers of the yanshanian boundary. the lower layers takes on the tectonic style of thrust fault and nappel. the upper layers hi step positive fault
2 、盆地燕山期構造界面上下不同構造層
具有完全不同
的構造樣式，構造界面下伏構造層呈現沖斷
褶皺、推覆構造樣式，構造界面上覆構造樣式為階梯狀正斷層，整體呈現「雙層」結構型式。
Santanghu basin, located in the edge of the southern siberian plate, has the double basements of the pre - cambrian crystalline basement and the palezoic metamorphic basement of volcanic - sedimentary rocks
三塘湖盆地位於西伯利亞板塊南緣，
具有前寒武紀結晶基底和古生代火山巖-碎屑巖
褶皺基底組成
的雙重基底。
The western hubei - eastern sichuan area is located at the junction belt between the eastern sichuan folded belt in the sichuan basin and xianexi folded belt, belong to eastern extended part, which is similar to the eastern - sichuan structure in many aspects. for example, they share a structural unit, resulting in the same sedimentary history and the same generation - reservoir - seal assembly as each other
鄂西渝東區處於四川盆地川東
褶皺構造帶與湘鄂西
褶皺帶
的接合部位，屬川東
褶皺帶東延組成部分，
具有與川東相似
的沉積發育史與生儲蓋組合；相同
的構造發育史與構造形式；類似
的天然氣藏類型與保存條件。
The traces of the bog were removed from it ; the creases left by the wet smoothed out : it was quite decent. my very shoes and stockings were purified and rendered presentable. there were the means of washing in the room, and a comb and brush to smooth my hair
泥沼
的印跡已經洗去，潮濕留下
的褶皺己經熨平，看上去很不錯了，我
的鞋子和襪子已洗得乾乾凈凈，很是象樣了，房子里有流洗
的工
具，有一把梳子和一把刷子可把頭發梳理整。
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。
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。
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。
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。
Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion
由於受區域構造長期作用
的影響，在北天山山前地區逐步發育形成了多排
褶皺背斜及活動斷裂，且運動方式
具有獨特性。
The a - c films were quantitatively analyzed by boxing dimension method. it indicates that with the fractal dimension increase, such surface of a - c film has more complicated microstructure, more and finer nanostructured grooves, so that it is able
隨著分形維數
的增大，薄膜
的表面
具有更加復雜
的結構，表面有更多和更精細
的具有納米尺度
的凹凸、皺
褶和缺陷結構，
具有更大
的吸附和容納氣體
的能力，從而提高水滴薄膜表面
的接觸角。
Effect of structure on cbm formation and destruction reflects in three aspects : geological developing history, fold and fracture. region where valid depth is smaller than 200m has no exploration value
構造對煤層氣藏的形成和破壞主要表現在地質發展史、褶皺、斷裂三個方面，其中上覆地層有效厚度小於200m的地區不具備勘探價值。
