斷裂點區 的英文怎麼說

中文拼音 [duànlièdiǎn]
斷裂點區 英文
breakpoint region
  • : Ⅰ動詞1 (分成段) break; snap 2 (斷絕;隔斷) break off; cut off; stop 3 (戒除) give up; abstai...
  • : 裂動詞[方言] (東西的兩部分向兩旁分開) open
  • : Ⅰ名詞1 (液體的小滴) drop (of liquid) 2 (細小的痕跡) spot; dot; speck 3 (漢字的筆畫「、」)...
  • : 區名詞(姓氏) a surname
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  1. Three stages of deformation can be distinguished from the cataclastic superposition of matrices that infilled the microcracks in cataclastic rocks, and two phas es of paleotectonic stress field from the typical conjugated shear joints by stereograms illustrating

    構造巖中膠結物和微隙充填脈反映了巖石碎變形的三次疊加。變形帶內發育兩期典型的共軛剪節理,但域分佈各有特,反映出變形的空間演化。
  2. The difficulties lie hi that there is any disturbance of yawp, character conglutination, and character rupture etc. the paper first presents some methods that adopt prior knowledge of the license plate, perpendicular projection, and minimum character area and so on

    車牌圖像的單字元分割即把車牌的整體域分割成單字元的域,以便后續進行識別,車牌字元分割的難在於噪聲和字元粘連、對分割的影響。
  3. Approach on break crossover point diastrophism direction of break coal intersecting line drawing in complex structure area

    復雜構造煤交線繪製法中錯動方向的探討
  4. The weishan - yongping copper - gold - polymetallic mineralization district in yunnan is tectonically located in the southern part of lanping basin in the middle part of changdu - simao block between lanchangjiang fault and jinshajiang - ailaoshan fault. more than 140 deposits and occurrences of gold, copper ( cobalt ), stibium, mercury, lead, zinc, iron etc. have been found in the area studied, and there are 4 medium - sized deposits among them

    雲南巍山-永平銅金多金屬礦化集中位於瀾滄江大與金沙江大、哀牢山大之間的昌都-思茅中間地塊中部的蘭坪盆地的南段,礦化集中內目前已發現金、銅(鈷) 、銻、汞、鉛、鋅、鐵等各種金屬礦床() 140處,其中達中型規模的礦床有4個。
  5. The investigation and study showed that caused by the influencing factors of unit of tectonics, structures of floor rock stratum, conditions of landform, seismic intensities, fault, thickness of malan loess, the distribution of seismic loess landslides is very asymmetrical, which mainly show shapes of patch, belt, line, and there are different development characteristics in different regions

    現場調查顯示,受大地構造單元、基底巖層結構、地形地貌條件、地震烈度、構造和馬蘭黃土臨空厚度等因素影響,地震黃土滑坡的展布形態較為復雜,在空間上分佈很不均勻,常表現為片狀、帶狀和線狀展布,並在不同域有不同的發育特
  6. By applying the theory and method of geological anomaly, it is focused on the analysis of the characters of major geological anomalies and their effect of mineralization in daye - jiurui region. the analysis result shows that the basement fault anomalies control a few major large hidden batholiths and their associated orefields ; that the anomalies of cover structure confine most cu - au deposits and fe - cu deposits within their scope ; that the geochemical anomalies and lithofacies - paleogeographical anomalies are major geological factors leading to trataboundness of some cu - au deposits ; that the anomalies of rock operties provide the favorable chemical and physical conditions for the ore - forming process, including the seepage, circulation, convergence and deposit of ore - bearing hydrothermal solution ; that the anomalous ctive stage of mesozoic magmatite is almost consistent with the major mineralization epoch of the fe, cu deposits, and the structure of multi - levels, and the zoning in magmatic system determine the spatial distribution of the mineralization system. then, based on the above analysis, a comprehensive variate, geological combination entropy, is brought forward for reflecting the complex degree of the combination of geological ore - controlling factors. after circumscribing the anomalies of geological combination entropy, the relations between the anomalies and ore deposits are determined

    從地質異常的角度,重分析了大冶九瑞地主要地質異常的特徵及其對成礦的影響.由分析可知:基底異常控制了本若干重要規模較大的隱伏巖基及伴生礦田,而蓋層構造異常控制銅金礦床和鐵銅礦床的空間位置;地層的地球化學異常和巖相古地理異常是造成一些銅金礦床層控性的主要地質因素;蓋層的巖性異常為含礦熱液的滲流、循環、聚集和礦質沉澱等一系列成礦作用提供了有利的物理和化學條件;中生代巖漿巖的異常活動期也是本主要的鐵銅成礦期,巖漿巖系統的多層分枝和分帶性結構控制了本成礦系統的三維空間分佈.在上述分析的基礎上,構置了地質組合熵作為反映控礦地質因素組合系統結構復雜程度的綜合變量,並圈定出組合熵異常,由此確定了綜合地質異常與礦床的關系
  7. Analyzing the propagation behaviors for open and close crack, the author gain that normal fault is more dangerous to earthquake than reverse fault and glide fault. 3. appling fracture mechanics to discuss reservoir - induce earthquake mechanism, the author observes the characteristic of surface crack and gains the stress intensity factor induced by the pressure of rock, water and osmosis

    針對庫層為表面紋這一特,研究水庫地震的,得出地應力作用下的應力強度因子、庫水作用下的應力強度因子和滲壓作用下的應力強度因子以及它們的應力強度因子之合,並且合理的解釋了構造型水庫地震的誘發機理。
  8. The result show, most of the medium - strong earthquakes faults are dip - slip reversed, distribution of the main stress p axis is sector from west to east ; there are large difference between kuche and baicheng region in seismic activities, but the characteristic of cluster is same in the two region ; the distribution of medium - strong earthquakes is nw direction in baicheng region, it show, there can have a concealed fault ; small earthquake clusters ' activities can reflect the effect that local medium - strong earthquakes to the secondary small structure around it

    結果表明:南天山東段中強震震源錯以傾滑逆為主,主壓應力p軸由西到東呈扇形分佈;相距較近的庫車與拜城地地震活動存在較大差異,但均存在明顯的成叢性分佈特;拜城地中強地震分佈呈北西向可能預示著該存在隱伏,小震群活動則可能反映了局部中強震對周圍次級小構造的影響。
  9. In order to make full use of advantages of high stress precision in iem and wide use of fem, zonal fem - iem is constructed to establish a foundation of method in viscoelastic interface mechanics

    為充分利用界面元法應力精度高、有限元法適用范圍廣的優,還建立了分界面元-有限元法列式,為粘彈性界面力學分析奠定了方法基礎。
  10. Multistage structural deformations are experienced in kongquehe area, the basical fault systems of nww - near ew, nne - near sn, nnw and nee are established, the fault movement has the characteristics of multistage and inheritance, in the area multi - structural deformations are experienced in sinian to early ordovician, early ordovician - silurian, jurassic cretaceous - caenozoic, etc. late structural deformation shapes are changed for different levels of formar structural layer, in which different deforming shapes are created and integrated overlying of deformation is induced

    摘要孔雀河地經歷了多期次的構造變形作用,形成了現今北西西近東西向、北北東近南北向、北北西向和北東東向基本體系,同時活動表現為多期性和繼承性的特;該經歷了震旦紀至早奧陶世、早奧陶世末志留紀、侏羅系、白堊紀新生代等多期構造變形作用,且後期的構造變形作用在不同程度上對前期的構造層的變形樣式有所改造,形成了有一定差異的變形面貌,造成變形的復合登加。
  11. This difference is caused not only by maturity but also by source rock. natural gas in baimiao area is mainly derived from tertiary source rock and carboniferous permian formation in qianliyuan sag, which is near the high point on lanliao fracture belt

    白廟地天然氣主要來源於前梨園窪陷第三系烴源巖和石炭?二疊系煤系地層,靠近蘭聊帶構造高,淺層es _ 2 ~下? es _ 3 ~ 2氣層具有較高的ar ~ ( 40 ) ar ~ ( 36 )比值,為煤型氣及混合氣。
  12. Several normal faults within the hainan fault zone constitute a fault - step zone and form a narrow and steep zone, which controlled the development and distribution of depositional systems in this area

    研究認為,海南帶的幾個北掉層構成階帶,形成湖盆邊緣陡且窄的地貌特,控制了該沉積體系的展布規律。
  13. Based on the characteristics of the quaternary tectonic activities of babaoshan - huangzhuang - gaoliying fault and the regional principal compressional stress direction and regional tectonic activities derived from the recent cross - fault displacement observation data in the capital area, we have analyzed the relationship between the fault movements at 7 cross - fault observation sites on the babaoshan - huangzhuang - gaoliying fault and the seismicity, conclude that the capital and adjacent area is soon to enter upon the next active period of earthquakes

    摘要根據八寶山黃莊高麗營第四紀地質構造活動特徵和利用首都圈地層位移最新的觀測資料求得的北京地域主壓應力方向和域構造活動特徵,分析了八寶山黃莊高麗營上7處跨層位移測層活動與地震活動的關系,得出了首都圈及鄰近地即將進入下一個地震活躍期的結論。
  14. Supported by remote sensing and cis, through image processing, information extracting and based on mathematic models of plural information, in this paper, some favorable gold areas in mian - ning and yan - yuan area have been predicted, and it achieved the following results : ( l ) through remote sensing image digital processing, we made high accuracy remote sensing images and image interpretion maps. constructed a geodatabase of mianning - yanyuan - xichang area, including basic data ( district. drainage, etc. ) and thematic data ( rupture, stratum, magmatic rock, etc. ). this will provide scientific evidences for work of this area in the future

    並取得了以下成果: ( 1 )通過遙感圖像數字處理,製作完成了實驗的高精度遙感影像地圖及遙感解譯圖,建立了冕寧-鹽源-西昌一帶空間數據庫,包括基礎數據(行政、地名、水系等)和專題數據(、地層、地質體等) ,為該進一步工作提供了科學依據; ( 2 )根據各個多元信息成礦預測模型的優缺,分析了不同預測模型的適用條件和范圍,確定了研究採用的數學模型。
  15. Through investigation and study about the geology and physiognomy of jingxingyan scene spots, the spots were proposed to be divided into several kinds according to its reason of formation, such as location advantage, rock basis, fracture constructions and efflorescence products

    摘要通過對浙江仙居景星巖景的地質、地貌進行考察和研究,發現景星巖景各景按其主要形成原因可分為:位優勢、巖石基礎、構造主導、風化產物等幾種類型。
  16. In this paper, false color photomontage with scale of 1 : 100000 treated by the remote sensing picture of xi ' an district in 2002 is the calculating base, and the basic theory of breakpoint method and the matlab software that is used to program and recognize the image are applied to divide the area of urban fringe in xi ' an

    在對西安城市邊緣的界定過程中,本文以西安地2002年1 : 100000的遙感圖像做成的假彩色合成影像圖為計算依據,運用「」分析法和信息熵兩種方法劃分了西安2002年的城市邊緣范圍。
  17. 2. the feature of geochemical primary halo in longshujiao ore segment shows that there is a positive abnormality of fi set of main chemical elements at 96 ~ 100 investigating line, longshujiao fault and fault 11 - 29, a east - north a positive abnormality of fs set of main chemical elements around 98 investigating line, big area positive abnormality of f4 set of main chemical elements in east ore segment and the feature of this abnormality is like the shape of the main ore - body in the west

    2 、龍樹腳礦段構造原生暈特徵分析顯示, f _ 1主元素因子組在96 100勘探線,龍樹腳至? 29號間出現一個因子得分高值異常; f _ 5因子組以98勘探線為中,因子得分值形成一個北東向高值異常; f _ 4因子組元素因子得分在東礦段形成大面積異常,異常特徵與西部主礦體地表展布相似。
  18. Meanwhile, the paper has analyzed the influences of fatigue, damnification, bend and liquid collision to sucker rod breaking as well, and suggested some positive measures to avoid sucker rod breaking according to the characteristics of sucker rod breakin in guangbei area of bamianhe oilfield

    同時,對于因抽油桿疲勞、損傷、撓曲、液擊對抽油桿的影響也進行了分析,並針對八面河油田廣北抽油桿的特提出了積極防治對策。
  19. The strain softening of dam body and foundation is the necessary condition for dam instability. according to observation data of dam cracks, a gray cusp catastrophe model is established to judge the stability of the crack. according to the slope observation data of a certain hydropower plant, a nonlinear dynamic model is developed by means of reversion and the lyapunov exponent spectrum, and the lyapunov information dimension are calculated for judgement of the stability of the slope

    ( 5 )基於變分原理,研究建立了能量形式的失穩準則,並說明壩體、巖基的材料具有應變軟化的性質,是大壩失穩的必要條件;並利用大壩的縫實測資料,建立了相應的灰色尖突變模型,由此判縫的穩定性;根據某水電站庫滑坡體的變形實測資料,反演其非線性動力學模型,進而計算lyapunov指數譜、 lyapunov信息維來判定邊坡的穩定性及穩定程度。
  20. There are n ' t late paleozoic - mesozoic structural layer in xiaoqinling, so taihua group upheaval area and its bilateral ruptures are critical sectors of investigation

    因此,本文研究的重段為小秦嶺太華群隆升帶及其南北兩側帶。
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