boundary fault 中文意思是什麼
boundary fault
解釋
邊界斷層-
The author suggests that the three lithosphere - scale faults, lancangjiang fault, jinshanjiang - ailaoshan fault and axis fault in the middle of the basin, are the main geological structures that control the formation of basin, magmatism and metallogenic congregate district. the anticline structure with an axis of triassic strata and the related fault system within the basin, and gonglang arch - shaped folding structure in the south of the basin are the geological structure controlling the formation of ore fields. junctions of two or more faults with different orientation, interlayer cataclastic structural zone and oxidation - reduction ( redox ) boundary were the favorable position for the formation of ore bodies
認為瀾滄江斷裂、金沙江-哀牢山斷裂及盆地中軸斷裂這三條巖石圈斷裂是主要的控盆-控巖（巖漿巖）構造及礦集區尺度的控礦構造；盆地中以三疊系為軸的背斜構造及相關的斷裂系統、盆地西南緣公郎弧形構造等是礦田尺度的控礦構造；多組斷裂的交叉、層間破碎帶及地層柱中的氧化還原界面是形成礦體的有利部位。 -
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。 -
The western margin can be divided by qingtongxia - wuzhong and zhongwei - zhongning fracture with east - west tending into three districts, north, middle and south distict. the north district includes zhuozishan and yinchuan graben and hengshanbu part by the boundary of zhengyiguan fault
將其分為北、中、南三區，其間分別以區域近東西向的青銅峽-吳忠和中衛-中寧斷裂帶相分隔。 -
The hanging wall of sag extended in southeast direction, with the tulage fault being the boundary fault. yinggete - bagemaode metamorphic core complex developed adjacent to northwest of chagan sag, which evolved from late jurassic to cretaceous with three - layer construction style. the kinematics mechanism of metamorphic core complex and chagan sag is a simple shear model, chagan sag extended and faulted as the metamorphic core complex rised
在查干凹陷西北側發育英格特?巴格毛德變質核雜巖帶，可能具有三層結構模式，其形成與演化時代為晚侏羅世末?白堊紀；該變質核雜巖與查干凹陷的運動學機制為統一的簡單剪切模式；在變質核雜巖隆升的同時，查干凹陷發生伸展斷陷。 -
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。 -
By means of kiba formation, k. ibt " and kibt2 segments analysis on the equivalent time stratigraphic framework, subtle traps will be predicted on stratigraphic traps and lithological traps. the results from the research indicated that : ( 1 ) this paper further indicates the control significance of southern boundary fault displacement component, which downthrown side forms syncline or anticline, and points out that 4 anticlines in south are adjustment zone and are the entering lake position of ancient river
本論文的主要認識和結論如下： （ 1 ）進一步認識南緣邊界斷層位移量對下降盤形成次凹或橫向突起的控制意義，認出南緣的4個突起是調節帶之所在，也是古河流入湖處。這種格局導致凹陷強烈分割，並以橫向搬運為主。 -
Both kinds of plate boundary are associated with fault systems, earthquakes and volcanism, but the kinds of geologic activity observed at the two boundaries are quite different
兩種板塊邊界均與地層系統、地震以及火山活動有關，但在兩種邊界處觀察到的諸般地質活動卻迥然不同。 -
In this paper we investigate and carry out boundary scan ^ internal scan and built - in self - test three dft technologies in the embedded microprocessor estarl and get satisfying result, the fault coverage is more than 96 %
本文針對嵌入式微處理器estar1的結構特點，研究並實現了邊界掃描、內部全掃描和內建自測試三種可測性設計技術，取得了良好的效果，故障覆蓋率達到96以上。 -
On the other hand, boundary - scan technique intelligent fault diagnostic method was applied to practice. for most digital system, devices with boundary - scan architecture are broadly used. only using four line or five line to connect pc parallel port with cut tap ( test access port ), all the ptvs can be loaded to cut and all homologous prvs can be taken back to intelligent fault diagnosis system
至於本文採用邊界掃描測試故障診斷技術，是考慮到本系統的通用性和簡潔性，因為對于大多數數字系統而言，具有邊界掃描結構的器件己廣泛應用，本文只需4條或5條信號線就能將pc機和被測邊界掃描電路連接起來，由此極大地簡化了智能故障診斷系統中為實現ptvs加載和prvs獲取而專門設計的介面板電路。 -
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
斷層的生長指數分析表明，依舒地塹內部的北西向斷裂與邊界斷裂的活動具有一致的規律性，都起到協調邊界斷裂演化發展的作用。 -
A physical model for describing the fault movement along plate boundary is proposed, i. e., the crust movement along plate boundary equals to the relative rigid plate motion plus negative dislocation distributions on the fault planes
提出了一種描述板塊邊界斷層運動的力學模型，即將板塊邊界的地殼運動表述為板塊的相對剛體運動加邊界斷層面上的負位錯分佈。 -
The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep. under the background of indian plate subducting under asia - europe plate, bachu forebulge was greatly affected by the development of southwest depression and awati depression. almost all of its structure reversed, and as a result of it, both of its south and north boundary migrated. according to its evolution history and its feature, the authors tentatively use both - side migration model to interpret the evolution of compound forebulge. since triassic, almost all the spheres above lithosphere synchronously became flexure. because transpressional stress field became increasingly strong, bachu forebulge continued uplifting and big faults formed. then, bachu uplift, as a whole, slipped upward along those big faults and showed migrating toward thrust zone in plane. in tectonic tranquility, the lithosphere bounded back and in consequence of it, bachu uplift slipped down and showed migration toward craton, at that moment negative inversion structures developed. while the forebulge migrated toward its south and north foredeep, it was very possible that locally extensional stress appeared in the forebulge
在印度板塊向歐亞板塊俯沖的大背景下，巴楚前緣斷隆受西南坳陷和阿瓦提凹陷的影響，新生代時構造體制發生反轉，邊界向南北遷移。根據其發育過程特徵，作者用復合前緣隆起兩端遷移模式對復合前緣隆起獨特的構造發育史進行了解釋：即三疊紀以來巖石圈各圈層同步撓曲變形。隨著擠壓應力場的增大，巴楚隆起在撓曲基礎上不斷抬升，形成幾條大型斷裂帶。 -
Different tectonic style exists in the upper and lower layers of the yanshanian boundary. the lower layers takes on the tectonic style of thrust fault and nappel. the upper layers hi step positive fault
2 、盆地燕山期構造界面上下不同構造層具有完全不同的構造樣式，構造界面下伏構造層呈現沖斷褶皺、推覆構造樣式，構造界面上覆構造樣式為階梯狀正斷層，整體呈現「雙層」結構型式。 -
According to the comparison result, the variance analysis will not be applicable when the allowance range has to be set flexibly according to specific operation requirements although it can achieve a high rate of fault detection. for example, when the allowance range of some particular component gets bigger, the variance analysis could not precisely define the new judgment boundary
比較后發現，方差特徵分析法雖然可以達到很高的故障檢測率，但不適用於元件容差需根據具體要求靈活設定的情況，例如當具體情況中某個元件的容差范圍變大時，用方差分析法卻不能準確地定出新的判斷界限。 -
Applying this model to the san andreas fault in southern california, which is the boundary between the pacific plate and the northern american plate ， the parameters of the physical model is determined by the inversion of the geodetic data of late 30 years in this area
應用該模型描述北美板塊與太平洋板塊邊界處的聖安德烈斯斷層帶，並用該地區近30年的大地測量數據反演了模型參數。 -
It can be concluded that : presently the eastern segment of qilianshan fault zone and its boundary region with zhuanglanghe fault and haiyuan fault is in an obvious background of strain accumulation ; lanzhou and linxia area near the southern segment of zhuanglanghe fault display a feature of strain accumulation in certain degree
分析結果表明：祁連山構造帶東段及與莊浪河斷裂、海原斷裂交匯區域目前可能具有相對高應變能積累背景；而莊浪河斷裂南段的蘭州、臨夏一帶反映一定程度的應變積累特性。 -
While there is no distict evidence to prove the tanlu fault ' s noted deep and dynamic behavior within the lower crust or even on the upper mantle. thus there still exists a necessary to research and check the understanding about the boundary ' s location and the dynamic background
作為一級構造單元分界線的紅河斷裂、怒江斷裂是超殼斷裂，而昌寧雙江斷裂顯示為低角度鏟式斷層，中下地殼無與之對應的速度異常，可能意味著該斷裂切割不深。 -
In the third part, the author analyses the cognitive foundation of the concept of compound fault, namely fuzziology in the pure science, which indicates that it ’ s normal that the boundary between the indirect intention and the recklessness is blurred and ambiguous. in the last but not the lest important part, the dissertation deals with some questions arising from the establishment of the concept of compound fault, for
由於我國現行刑法第14條、第15條僅明確規定了故意與過失兩種罪過形式，因此復合罪過形式是一個沒有法定名份的理論概念;雖然如此， 「復合罪過形式」卻是一個有實際內涵的實然性概念。 -
Bachu arch is a large back - thrust uplift. tectonic evolution of its large boundary fault fracture have relation with oil / gas distribution involuntarily. its large boundary fault fracture is basement rift formed in late hercynian period and strongly actived in late himalayan period. oil / gas distribution of bachu - markit have relation with fault interspace distribution. so, this paper also discussed interspace distribution and movement stage of fault
巴楚隆起是一個大型背沖斷隆，其邊界大斷裂的形成演化自然關繫到本區的油氣分佈，隆起的邊界大斷裂多是海西晚期形成的基底斷裂，后在喜山期強烈活動，兼具壓扭走滑性質。 -
1 based on the analysis of sedimentary structure and sedimentary energy, the facies model was founded. pucheng oil field is tightly adjacent to the boundary fault of dongpu depress, and it is easy to develop fan - delta and sub - fan on this location. in fact it is easy to find the sediment supply of the studying area is mainly from eastern high through the thickness map and its sand - content map
在研究層段共劃分長期旋迴1個、中期旋迴6個和短期旋迴27個（短期旋迴規模太小，僅能在巖心上識別） ，通過測井曲線的基準面識別和對比，確定了地層的分佈，結合基準面旋迴內可容空間的變化，對其沉積演化進行了分析。
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