滑動斷層 的英文怎麼說
中文拼音 [gǔdòngduàncéng]
滑動斷層
英文
glide fault- 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...
- 斷 : Ⅰ動詞1 (分成段) break; snap 2 (斷絕;隔斷) break off; cut off; stop 3 (戒除) give up; abstai...
- 層 : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
- 滑動 : slither; slippage; slipping; slide; sliding; run; sliding movement [motion]; glide; slump滑動閘門...
- 斷層 : fault; slip; slicle; fracture; dislocation
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There are typical laminated structure, soft sedimentary - slipping deformed structure, syngenetic brecciated structure in the ore which are the mirror of syngenetic sedimentation. the other type of ore has the charactristic of epigenetic mineralization, which is called as telescoped ore. the ore occurs in vein, pocket, lensoid and bedd
礦石中發育典型的紋層狀構造、軟沉積滑動變形構造、同生角礫構造等反映同生沉積特徵的礦石構造;另一類礦石具有明顯的後生成礦特點,稱之為疊生改造型礦石,礦石產于脈狀、囊狀、透鏡狀及似層狀礦體中,與燕山期巖漿巖及斷裂裂隙構造關系密切。Based on the bedding features of weak intercalations in sandstone plates near the top of underground cavity, the probable failure scale of bedding sliding, the probable settlement, the folding places and the critical length of sandstone beams are computed seperately, then the stability of underground cavity is analysed
針對地下工程頂部層狀砂巖中存在順層發育軟弱夾層的情況,分別對開挖后可能出現的層間滑動破壞范圍、巖板的沉降、折斷和臨界長度進行計算,並分析其穩定性。One mode is slippage along the discontinuity provided by the lubricated fault plane.
其中一種方式是沿著潤滑的斷層面所形成的間斷面而發生滑動。On the east terrace - fault slope of the depression, the sedimentary mode of fan - shaped delta - slump turbid fan - deep lake facies are developed. on the long axial direction of fula depression, the southeastern groove was filled with a large scale delta which was the main sources, the other little delta limited by the 3 syndepositional fault was distributed down the slope edge of the northern sub - depression. this stage developed a favorable oil sources, reservoir and regional seal which formed the good matching relations of generation, reservoir and seal in the time - space zone
Abugarbra組的sc和sd層序發育在邊界斷層和同沉積斷層活動劇烈、湖盆擴張期,凹陷中心發育半深湖-深湖相沉積,在凹陷陡坡發育近岸水下扇,斷階緩坡帶發育扇三角洲?滑塌濁積扇?深湖相組合,長軸凹槽和北部次凹的北部緩坡帶發育三角洲體系,此層位是有利生油層和巖性圈閉發育層段。The kinematics of sudden faultslip have not yet been directly observed.
突然的斷層滑動的運動情況迄今還沒有人作過直接觀測。The silent earthquakes may then take place when a batch of fluid from the slab is working its way up ? as the fluid passes, it will unclamp the fault zone a little bit, perhaps allowing some slow slip
這是因為當水通過斷層帶的片刻,會微微地搖撼一下斷層帶,這或許就是引發輕微滑動的原因。The existence of silent earthquakes gives scientists a completely new angle on the slip process by permitting the detailed study of fault zones through every stage of their movement
然而,無聲地震的存在卻提供科學家一個全新的角度,來看待斷層滑動的過程,讓他們對斷層帶運動的每個階段做更仔細的研究。Variations in rock type and structure in the fault zone would entail variations in slippage rate along the trace.
斷層區的巖石類型和構造的不同將會引起沿斷痕滑動的速率的變化。On the portion where slippage is small or nonexistent, surface offsets should be a maximum and of the order of the throw at depth.
在斷層中滑動很小或不存在有滑動的部位,表面錯距可能最大並和深部差動屬同一量級。Along fault zones in particular, displacement may occur by slow, secular, differential slippage as well as by sudden rupture.
特別是沿著斷層區,位移既可能以緩慢的,持久的、有差異的滑動發生,也可能以突然破裂發生。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。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。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。Sudden rupture and displacement occurs with normal, reverse, strike-slip, or oblique-slip faulting.
突然破裂和位移伴隨正、逆、走向滑動或斜向滑動斷層作用而發生。The ne - strike compressional faults are not intersected with the ew ma in fault zone, but a kind of transform structure resulted from its right lateral strike slip, and one of the typical example is the mesozoic thrust systerm in the northeast side of the main fault in western liaoning
在青龍斷裂帶兩側,分佈有許多北東向壓性斷層,它們與東西向主斷裂帶不是簡單的切割關系,而是東西向主斷裂帶右行走滑活動中的分支斷裂,位於青龍斷裂帶北東側的遼西地區中生代逆沖推覆構造,也是青龍斷裂帶在右行走滑作用下,因構造方向的改變發生構造轉換的結果。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。The cover faults in daqing region are mainly developed in formation of huoshiling member late jurassic and its cover formations. according to their formation period, activity characteristics and penetrating relationship, four types of faults were divided, that is fault - depression faults, depression faults, inverted - strike - slip faults and inverted - extension faults ; according to the activity history of the faults, five types of faults were divided, that is long - term active faults, early active faults, early - medium - term active faults, medium - term active faults and terminal active faults
大慶地區內發育在晚侏羅世火石嶺組及其以上的沉積蓋層中的蓋層斷裂,依斷層形成時期、活動特徵及切割層位可將蓋層斷層細分為四種類型,即斷陷期斷裂、坳陷期斷裂、反轉走滑斷裂和反轉張性斷層;按其活動歷史可以分為五種類型:即長期活動斷層、早期活動斷層、早-中期活動斷層、中期活動斷層和晚期活動斷層。The importance of deciphering fault slip is difficult to overstate because when faults slip quickly, they can cause immense damage, sometimes at a great distance from the source
要去了解、解釋斷層滑動的重要性是無庸置疑的,因為一旦斷層快速滑動,將會造成巨大的災情,有時發生位置甚至離震源還有一大段距離。The fault zone passes through the offshore between the changdong islands and the dazhudao island, and consists of a group of nw trending faults, which are dominated by normal and reverse slips with strike - slip component
該斷裂帶由一系列北西走向的次級斷層組成,主體在長島至大竹島之間的海域,多數斷層以正斷兼有走滑運動為主,部分斷層具有逆沖運動性質。Ma jin and ma shengli, 1987, the role of fault material in fault movement and seismological significance, earthquake research in china, 1, 3
馬勝利,馬瑾, 1988 ,高溫高壓下石英和方解石斷層帶的摩擦滑動性狀,地震學報, 10 , 1 。分享友人