fault n. 1.过失,过错;罪过,责任。 2.缺点,缺陷,瑕疵。 3.(猎狗的)失去嗅迹。 4.【电学】故障,误差;漏电;【地质学;地理学】断层。 5.【网球】发球出界;犯规。 Faults are thick where love is thin. 〔谚语〕一朝情义淡,样样不顺眼。 fault detection 【机械工程】探伤。 The fault is his own. 这是他自己的错。 a grave fault in a theory 理论上的重大缺陷。 a fault in the machine 机械故障。 image fault 【物理学】像差,影像失真。 numerical faults 数值误差。 a fault on the right side 因祸得福。 be at fault 1. (猎犬追捕猎物等时)失去嗅迹,踌躇不前;不知所措,正在为难。 2. 出毛病,有故障。 3. = in fault (My memory is at fault . 我想不起来了)。 find fault in 看出…缺点。 find fault with 找…的岔子。 have no fault to find with 无错可寻。 hit off a fault (猎狗)闻出(曾一度错失的)嗅迹。 in fault 有过错,有责任 (Who is in fault 是谁的不是?)。 to a fault 过度,极端 (He is kind to a fault. 他过分老实)。 whip a fault out of sb. 鞭打某人使之改过。 with all faults 不保证商品没有缺点。 without fault 〔古语〕无误,确实。 vi. 1.【地质学;地理学】产生断层;有断层余迹。 2.发球出界;犯规。 3.〔方言〕责备,挑剔。 4.〔古语〕犯错误,做错。 vt. 1.找…的岔子,挑剔;〔方言〕责备。 2.【地质学;地理学】使产生断层。 3.把…做错。 He faulted my speech in two ways. 他认为我的讲话有两点不妥。 fault one's performance 表演发生失误。
On the basis of the characteristics of sequence stratigraphy of the cenozoic in puwei sag , dongpu depression , the sequence stratigraphic framework of the cenozoic is set up , including two supersequence sets which is fault depression filling supersequence sets of the eocene , and depression filling supersequence sets of the tertiary 根据东濮凹陷濮卫洼陷新生界层序地层的发育特征,建立了濮卫洼陷新生界层序地层格架,将濮卫洼陷新生界概括为一个盆地充填序列,包括古近系凹陷充填超层序组和新近系坳陷充填超层序组。
This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement , whose tectonic deformation and magma intrusion is fiercely , and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian , it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area , such as a - granite ' s stock , batholiths and diabase ' s dike . there are many fault depressions possible 按照不同构造层,研究了各构造层的构造特征:基底构造层:受早海西期构造作用的影响,与准噶尔洋盆俯冲闭合、而后陆-陆碰撞的区域挤压构造作用有关,为一构造变形和岩浆侵入活动强烈的古生代褶皱基底。二叠系构造层:受中海西区域性伸展断陷作用的影响,盆地及其周缘地区发育与伸展构造有关的构造-岩浆组合,如呈岩株、岩基状侵位的a型花岗岩以及呈岩墙状侵位的辉绿岩等。
Due to the multi - period tectonic movement and evolution of mechanical mechanism , syndeposition structures occur extensively in jiyang sag , the base of the sag subsided alternatively during the fault depression , which resulted in sinking of top bending and complicated block structure accordingly , reconstructed the syndeposition intensively , and produced the special structural landscape in combination with all levels of faults and sedimentary formations within it 摘要济阳坳陷由于受到多期构造运动的影响,在前第三系古地形高点背景上广泛发育同沉积背斜构造,然而由于坳陷在断陷期基底滚动式沉降,造成挠曲顶部的塌陷,形成复杂的块断结构,使本区同沉积构造发生强烈改造,往往与各次级断层或沉积地层相复合,表现出独特的构造景观。
Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward , which evolved from late jurassic to cretaceous . the extensional simple shear model of the chagan fault depression is established . the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure 讨论了查干凹陷及邻区中-新生代盆地构造演化及其地球动力学特征,三叠纪(印支期)为陆内造山作用与地壳增厚、隆升剥蚀阶段;侏罗纪(燕山早期)为造山后造山带的局部伸展垮塌阶段;白垩纪(燕山晚期)为造山期后大规模伸展垮塌作用与伸展盆地的发育阶段;新生代(喜山期)为远距离碰撞效应与弱挤压挠曲性质的稳定大陆内坳陷的发育阶段。
It could be divided into six paleogeotemperature evolution stages from early cretaceous to recent based on the result of apatite fission - tracks analysis ; subsidence - buried history analysis shows that chagan experienced fault depression stage during early cretaceous bayingebi - suhongtu period , transional stage from fault depression to sag in yingen period , and sag stage since wulansuhai stage 磷灰石裂变径迹模拟分析结果认为早白垩世至今大致可分为6个古地温演化阶段;沉降?埋藏史模拟揭示查干凹陷经历了早白垩世巴音戈壁?苏红图期的断陷期、银根期的断?坳陷转化期和晚白垩世乌兰苏海期以来的坳陷期。
This paper studies cretaceous volcanics distribution , rock types , tectonic setting and reservoir characteristics in the western depression of liaohe fault depression through statistics of compound logging data , core observation , thin section identification , cathodeluiminescence , scanning electron microscope , x - ray diffraction analysis , image analysis , rock chemical analysis , isotope age testing , and inclusions temperature testing 摘要通过全区综合录井资料的统计、大量的岩心观察,并利用薄片鉴定、阴极发光、扫描电镜、 x衍射分析、图像分析、岩石化学分析、同位素年龄测定、包裹体温度测定等10余种方法,对辽河断陷西部凹陷白垩纪火山岩分布、岩石类型、岩石系列、形成的构造背景及储层特征进行了研究。
It is therefore proposed in this paper to strengthen the exploration of such wide and deep subsags as chagannuoer and hongqi subsags , to lay emphasis on the exploration of superposed and residual fault depression , and to pay attention to the discovery of various oil and gas reservoirs including metamorphic buried hills , fracture slope breaks , and volcanic rocks , etc 因此,指出下一步应加强类似查干诺尔,红旗等宽深洼槽的勘探,重视具叠合型和残留型断陷的勘探,注重寻找包括变质岩潜山,断裂坡折带、火山岩等在内的各类油气藏。
Tertiary structures are developed in mesozoic - palaeozoic tectonic settings , the general framework is faulted depression faulted in the north and onlapped on the south and arch bounded by faults . they are controlled and affected by three sets of large successive - active faults ( nw , ne and nee strike ) , they are successive and segmented , with multiples types and zoning distribution 第三系的构造是在中、古生界构造的背景上发育起来的,它以北断南超的箕状断陷和断层为界的凸起为总的构造格架,受北西、北东和北东东向三组继承性活动大断层的控制和影响,构造具有继承性和分割性、类型具有多样性、分布具有分层分带性。
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 查干德勒苏凹陷属于银根?额济纳旗盆地东北端查干德勒苏坳陷内的一个次级构造单元。其基底为古生代时期华北板块、塔里木板块和哈萨克斯坦板块交接部位的陆缘或岛弧褶皱带,具有古生代造山带的性质。
With an area of 5300 km2 , dongpu depression is located in the southwest of lin - qing depression , bohaiwan basin , bounded with lu - xi uplift by lan - liao fault in the east , with nei - huang uplift by chang - yuan fault in the west , with lan - kao heave by the north feng - qiu fault in the south , with xin country depression by ma - ling fault in the north , while spreading along nne defection , taking on the forms of being wide in the south , and narrow in the north . it is a rift fault depression basin with the characteristics of striking , with the basement being the paleozoic and mesozoic , and the capping beds being the cenozoic 东濮凹陷位于渤海湾盆地临清坳陷西南端,东侧以兰聊断裂为界与鲁西隆起为邻,西侧以长垣断裂为界与内黄隆起相接,南以封丘北断层为界与与兰考凸起相邻,北以马陵断层为界与与莘县凹陷相望,是以古?中生界为基底,以新生界为盖层,古近纪形成的拉分走滑?裂谷型箕状断陷盆地。