slip fault 中文意思是什麼
slip fault
解釋
滑斷層-
4 ) analyses boundary faults of the cenozoic longmenshan foreland basin, and thinks the basin boundary faults, being active fault, are thrust and dextral strike - slip. so the longmenshan foreland basin is dextral strike - slip foreland basin
4 )通過對新生代龍門山前陸盆地邊界斷裂的考察分析,認為盆地邊界斷裂具逆沖推覆及右旋走滑作用特點,為活動斷裂。 -
It is believed that three northeast - striking dextral slip fault zones, i. e. the baxian - shulu - handan fault zone, the huanghua - dezhou - dongming fault zone, and the linyi - huanghekou fault zone, are the result of the tectonic transform of paleogene extending to neogene - quaternary laterally slipping of north china plain rift systems, which extend along the central axis of rifts and accord with the quaternary centers of subsidence as the main seismic structures within the rifts
認為壩縣束鹿邯鄲斷裂帶、唐山河間磁縣斷裂帶和黃驊德州東明斷裂帶3條北東向右旋走滑斷裂帶為華北平原裂谷系從早第三紀伸展拉張作用進入晚第三紀第四紀走滑剪切拉張作用的產物,這3條斷裂帶分別位於3個北東向坳陷帶中部,並構成了第四紀沉降中心,與營口濰坊斷裂帶起構成華北平原內的主要強震構造。 -
Especially interesting is the serpentinous peridotite in this belt occurred as lense blocks of various sizes, and superimposed with other geological masses with faults, and in combine to constitute the mixture. system in the belt. five tectonic stage can be discerned in this area : ( 1 ) south - north ward overthrust ; ( 2 ) sinistral strike - slip ( 3 ) dextral strike - slip ( 4 ) south - north ward overthrust ( 5 ) northeast, northwest late stage fault
本區上述的結構構造特徵先後經歷了五期構造作用,依次為: ( 1 )南北向逆沖推覆; ( 2 )左行走滑; ( 3 )右行走滑; ( 4 )南北向擠壓推覆; ( 5 )北東向、北西向晚期斷裂; -
Strike - slip model for altyn tagh fault developed since late mesozoic
晚中生代以來阿爾金斷裂的走滑模式 -
The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang, which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw, came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin, i. e. the strike - slip and stretch processes of baigezhuang fault
同時,用三維地震資料進行區域構造解釋分析,論述了柏各莊地區的構造樣式,是中新生代渤海灣裂谷盆地的幕斷陷發育階段,同時由於盆地內凸起邊界?柏各莊斷層的走滑兼伸展作用,使柏各莊凸起的中生界形成壘、塹斷塊群構造樣式,發育一系列ne ( nee )向,傾向nw或sw的正斷層。 -
The radiocarbon ages of charcoal and their implication derived from ciergou site along the haiyuan strike - slip fault
永定河上游晚更新世晚期以來的堆積階地年代測定 -
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。 -
Sinistral strike - slip faults along the southern alashan margin and eastwards extending of the altun fault
阿拉善地塊南緣的左旋走滑斷裂與阿爾金斷裂帶的東延 -
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 paper gives a mechanical and history analysis on the characteristic of laojunshan metamorphic core complex in southeastern yunnan and its structural environment, and considers that metamorphic core complex is actually a nuclear column of a vortex structure, which was caused by the wenshan ? malipo strike - slip fault
通過滇東南老君山變質核雜巖特徵及周圍構造環境的力學分析及歷史分析認為,該變質核雜巖實質上是旋扭構造的砥柱,而旋扭構造又源於文山?麻栗坡斷裂的走滑運動,拆離伸展構造晚于旋扭構造。 -
In himalayan, the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation. in eastern ore belt, ore - controlling is mainly strike - slip fault and fold ; but in western ore belt, it is block
喜馬拉雅運動第一期45ma盆地掀斜;第二期23ma以差異隆升剝蝕為主;第三期4ma為脆性變形期,東礦帶近盆邊以走向斷裂及褶皺控礦為主,西礦帶為斷塊控礦。 -
Strik - slip fault
橫移斷層 -
Recent evidence and of the tangdong tectonic zone strike - slip fault in qikou depressed basin and it ' s significance in exploration
歧口凹陷唐東走滑斷裂存在證據及勘探意義 -
Antilistric dip slip fault
反鏟狀傾滑斷層 -
Strike - slip fault
走滑斷層 -
The mesozoic - cenozoic intracontinental strike - slip fault system and the associated hydrothermal uranium mineralization in the border area of eastern hunan and western jiangxi provinces
湘贛邊區中新生代走滑斷裂系統及對熱液鈾成礦作用的控制 -
Mesozoic - cenozoic continental strike - slip fault system and its roles on uranium mineralization in hunan and guangxi, china
湘桂地區中新生代走滑斷裂系統對鈾成礦的控製作用 -
Dip slip fault
傾移斷層 -
Some controversy has been put on aheqi fault, our data shows it is a ne trending left lateral strike slip fault, but its activity is weak
阿合奇斷裂是一條引起爭議的斷裂,我們收集的資料表明它是一條走向北東東的左行走滑斷裂,但它的活動性不是很強烈。
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