fault n. 1.過失,過錯;罪過,責任。 2.缺點,缺陷,瑕疵。 3.(獵狗的)失去嗅跡。 4.【電學】故障,誤差;漏電;【地質(zhì)學;地理學】斷層。 5.【網(wǎng)球】發(fā)球出界;犯規(guī)。 Faults are thick where love is thin. 〔諺語〕一朝情義淡,樣樣不順眼。 fault detection 【機械工程】探傷。 The fault is his own. 這是他自己的錯。 a grave fault in a theory 理論上的重大缺陷。 a fault in the machine 機械故障。 image fault 【物理學】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)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 . 我想不起來了)。 find fault in 看出…缺點。 find fault with 找…的岔子。 have no fault to find with 無錯可尋。 hit off a fault (獵狗)聞出(曾一度錯失的)嗅跡。 in fault 有過錯,有責任 (Who is in fault 是誰的不是?)。 to a fault 過度,極端 (He is kind to a fault. 他過分老實)。 whip a fault out of sb. 鞭打某人使之改過。 with all faults 不保證商品沒有缺點。 without fault 〔古語〕無誤,確實。 vi. 1.【地質(zhì)學;地理學】產(chǎn)生斷層;有斷層余跡。 2.發(fā)球出界;犯規(guī)。 3.〔方言〕責備,挑剔。 4.〔古語〕犯錯誤,做錯。 vt. 1.找…的岔子,挑剔;〔方言〕責備。 2.【地質(zhì)學;地理學】使產(chǎn)生斷層。 3.把…做錯。 He faulted my speech in two ways. 他認為我的講話有兩點不妥。 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斷層駕掌寺大斷裂時正時逆的特點,解決了深淺層構(gòu)造圈閉差別大的問題。
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)展與控礦過程,都是在這次地殼運動過程中完成的。
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致郯廬斷裂帶以西自北向南發(fā)育了3個北西向斷塹系,即北部的渤海斷塹系中部的濟陽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以來的新生代盆地格局。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致郯廬斷裂帶以西自北向南發(fā)育了3個北西向斷塹系,即北部的渤海斷塹系中部的濟陽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以來的新生代盆地格局。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)合實驗測試,對礦床的礦體、礦石、礦床成因等特征進行了研究,深化了礦床多階段多期次復合成因的認識,發(fā)現(xiàn)了含礦斑巖體。