at fault 感到困惑, 有故障; 有錯(cuò); 有過(guò)失; 有毛病; 罪有應(yīng)得
fault n. 1.過(guò)失,過(guò)錯(cuò);罪過(guò),責(zé)任。 2.缺點(diǎn),缺陷,瑕疵。 3.(獵狗的)失去嗅跡。 4.【電學(xué)】故障,誤差;漏電;【地質(zhì)學(xué);地理學(xué)】斷層。 5.【網(wǎng)球】發(fā)球出界;犯規(guī)。 Faults are thick where love is thin. 〔諺語(yǔ)〕一朝情義淡,樣樣不順眼。 fault detection 【機(jī)械工程】探傷。 The fault is his own. 這是他自己的錯(cuò)。 a grave fault in a theory 理論上的重大缺陷。 a fault in the machine 機(jī)械故障。 image fault 【物理學(xué)】像差,影像失真。 numerical faults 數(shù)值誤差。 a fault on the right side 因禍得福。 be at fault 1. (獵犬追捕獵物等時(shí))失去嗅跡,躊躇不前;不知所措,正在為難。 2. 出毛病,有故障。 3. = in fault (My memory is at fault . 我想不起來(lái)了)。 find fault in 看出…缺點(diǎn)。 find fault with 找…的岔子。 have no fault to find with 無(wú)錯(cuò)可尋。 hit off a fault (獵狗)聞出(曾一度錯(cuò)失的)嗅跡。 in fault 有過(guò)錯(cuò),有責(zé)任 (Who is in fault 是誰(shuí)的不是?)。 to a fault 過(guò)度,極端 (He is kind to a fault. 他過(guò)分老實(shí))。 whip a fault out of sb. 鞭打某人使之改過(guò)。 with all faults 不保證商品沒(méi)有缺點(diǎn)。 without fault 〔古語(yǔ)〕無(wú)誤,確實(shí)。 vi. 1.【地質(zhì)學(xué);地理學(xué)】產(chǎn)生斷層;有斷層余跡。 2.發(fā)球出界;犯規(guī)。 3.〔方言〕責(zé)備,挑剔。 4.〔古語(yǔ)〕犯錯(cuò)誤,做錯(cuò)。 vt. 1.找…的岔子,挑剔;〔方言〕責(zé)備。 2.【地質(zhì)學(xué);地理學(xué)】使產(chǎn)生斷層。 3.把…做錯(cuò)。 He faulted my speech in two ways. 他認(rèn)為我的講話(huà)有兩點(diǎn)不妥。 fault one's performance 表演發(fā)生失誤。
The ground simulation device base d on fault diagnosis expert system for program control fault simulation and data acquisition instrument is introduced 描述了地面模擬設(shè)備的組成和應(yīng)用于故障診斷地面模擬設(shè)備的專(zhuān)家系統(tǒng)。
The structure model shows the sometimes normal and sometimes reverse characteristics of jiazhangsi fault, which is the control fault of the reservoir 構(gòu)造模型清晰地展示了控藏?cái)鄬玉{掌寺大斷裂時(shí)正時(shí)逆的特點(diǎn),解決了深淺層構(gòu)造圈閉差別大的問(wèn)題。
At the same time, pulsating compressive force due to the crust movement including earthquake also made the crystallized rock ruptured and form ore control fault fracture and the host fracture 殘漿的形成與排出,控礦構(gòu)造的發(fā)生、發(fā)展與控礦過(guò)程,都是在這次地殼運(yùn)動(dòng)過(guò)程中完成的。
In this paper, a pwm-controlled fault current limiter is proposed . it is composed of a limiting reactor and a compensator capacitor, which is in parallel with a pulse width modulation ( pwm ) switched reactor 本文在總結(jié)前人研究成果的基礎(chǔ)上,提出了一種基于脈寬調(diào)制原理(pulsewidthmodulation,縮寫(xiě)為pwm)技術(shù)的故障限流器(pwm-fcl)。
The fault at the east boundary of tangyuan fault basin is a basin-controlling fault, and the faults at both the east and the west boundaries of fangzheng fault basin are also a basin-controlling fault, with the west boundary fault at fangzheng being the major one 斷層的生長(zhǎng)指數(shù)分析表明,依舒地塹內(nèi)部的北西向斷裂與邊界斷裂的活動(dòng)具有一致的規(guī)律性,都起到協(xié)調(diào)邊界斷裂演化發(fā)展的作用。
The fault at the east boundary of tangyuan fault basin is a basin-controlling fault, and the faults at both the east and the west boundaries of fangzheng fault basin are also a basin-controlling fault, with the west boundary fault at fangzheng being the major one 斷層的生長(zhǎng)指數(shù)分析表明,依舒地塹內(nèi)部的北西向斷裂與邊界斷裂的活動(dòng)具有一致的規(guī)律性,都起到協(xié)調(diào)邊界斷裂演化發(fā)展的作用。
Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin-controlled faults, tanlu fault zone strike slip to develop the three nw-trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben . based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene . the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull-apart basin in cenozoic time . the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin-controlled faults in the different depresses in bohai basin . the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin 根據(jù)中生界上侏羅統(tǒng)和下白堊統(tǒng)地層和控盆斷裂分布分析,中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導(dǎo)致郯廬斷裂帶以西自北向南發(fā)育了3個(gè)北西向斷塹系,即北部的渤海斷塹系中部的濟(jì)陽(yáng)斷塹系和南部的魯西南斷塹系。從區(qū)域資料綜合分析,渤海灣盆地的基本格局是早第三紀(jì)以來(lái)的新生代盆地格局。渤海灣盆地的形態(tài)構(gòu)造和沉積特征及熱流值分布表明該盆地在新生代為拉分盆地。
Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin-controlled faults, tanlu fault zone strike slip to develop the three nw-trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben . based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene . the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull-apart basin in cenozoic time . the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin-controlled faults in the different depresses in bohai basin . the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin 根據(jù)中生界上侏羅統(tǒng)和下白堊統(tǒng)地層和控盆斷裂分布分析,中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導(dǎo)致郯廬斷裂帶以西自北向南發(fā)育了3個(gè)北西向斷塹系,即北部的渤海斷塹系中部的濟(jì)陽(yáng)斷塹系和南部的魯西南斷塹系。從區(qū)域資料綜合分析,渤海灣盆地的基本格局是早第三紀(jì)以來(lái)的新生代盆地格局。渤海灣盆地的形態(tài)構(gòu)造和沉積特征及熱流值分布表明該盆地在新生代為拉分盆地。
The paper not only studies the mircostructure, malcrostracture features of ore-controlling fault system and kinemafic analysis but also deeply states the breccia pipe structure . lt considers that yinshan lead-zinc deposit is controlled by three-level structure condition . the ne-trending left-laterl structure movement is mainly controlling factor 在野外調(diào)查基礎(chǔ)上結(jié)合實(shí)驗(yàn)測(cè)試,對(duì)礦床的礦體、礦石、礦床成因等特征進(jìn)行了研究,深化了礦床多階段多期次復(fù)合成因的認(rèn)識(shí),發(fā)現(xiàn)了含礦斑巖體。