斜斷裂 的英文怎麼說

中文拼音 [xiéduànliè]
斜斷裂 英文
diagonal fracture
  • 斜 : 形容詞（跟平面或直線既不平行也不垂直的） oblique; slanting; skew; bevel; diagonal; askew; inclined; tilted
  • 斷 : 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 : 裂動詞[方言] （東西的兩部分向兩旁分開） open
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  1. Stability of rock slopes is generally controlled by the structure of rock masses, especially the soft structure surfaces. analysis of rock mass structures is a key to establish geological models and numerical simulation and a foundation to assess the stability of rock slopes. the weak structure surfaces are mainly bedding planes, faults, joints, schistosity plane and contact zones of intrusive bodies. since they are different in genesis and scale, the rock masses are different in features and mechanical intensities. based on the combination of rock structure bodies, 15 basic modes of deformation and failure of rock slope are systematically summarized. the deformation and failure of rock masses actually result from the recombination and rearrangement of these rock bodies. there are 11 types of rock mass structures and various deformation and failure of bank slopes are present in the reservoir area of the three gorge project

    巖體結構，特別是軟弱結構面對基巖斜坡變形與破壞具有顯著的控製作用，巖體結構模式分析是建立斜坡地質模型和數學模型的關鍵和評價斜坡穩定性的基礎。巖層層面斷裂構造節理裂隙片理與劈理以及侵入體和圍巖的接觸帶等是控制基巖斜坡穩定的軟弱結構面，這些成因不同大小不一的結構面將巖體分割成性質各異力學強度不均的各種巖體結構體，構成了15種基巖斜坡變形破壞的巖體結構基本模式。不同結構體的重新組合與排列是斜坡失穩的內在原因。
  2. The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement

    其後的繼承性活動在斷裂帶內形成碎裂程度最強達到碎裂巖的碎裂巖系列構造巖，變形帶兩側發育兩組典型的共軛剪節理；第二次在晚白堊世?始新世，斷裂在北東?南西向近水平擠壓作用下右行張扭性活動，斷裂帶兩主斷裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶，而斷裂在巖體區也發育兩組典型的共軛剪節理，斷裂內形成初碎裂巖為主的構造巖；第三次是喜山期以西側抬升、東側下降的強烈升降為主的活動，在基巖中，主斷層兩側圍巖出現微破裂。
  3. 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. ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin

    （ 6 ）論文探討了賽什騰? ?錫鐵山斜向逆沖推覆構造的地質意義，認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的結果，該認識對于研究柴北緣區域構造格局、盆山關系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義，對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。
  5. Sxotf is recognized in the northern qaidam based on the analysis of structures of area. this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge, fault breccia and fault cleavage. fault hanging wall consists of sertengshan - xitieshan napple, which is distribution in dextral en echelon. fault footwall consists of youcangshan formation in neogene

    本文在對賽什騰? ?錫鐵山斜沖斷裂詳細地段構造解析的基礎上，結合盆地的沉積特徵、地球物理資料等對該斜沖斷裂的幾何學、運動學及形成時代進行了研究，論文著重探討了賽什騰? ?錫鐵山斜沖斷裂的地質意義。
  6. The studied deposit area is located on a monocline geotectonic unit divided by several groups of faults. therefore, the secondary widen transverse and lognitudinal drapes may have great influence on ore forming and location

    礦區基本構造為一個被幾組斷裂破壞的單斜構造，其上發育的次一級的開闊型橫向和縱向褶皺對礦床的形成和空間定位起著十分重要的作用。
  7. The sankeng geothermal field is located on the northeastern side of the wuchuan - sihui deep fault and in the sankeng synclinal karstic basin

    摘要廣東三坑地熱田位於吳川四會深大斷裂帶的東北側，三坑向斜巖溶盆地內。
  8. It is shown that deep abnormal high pressure confined area ( abnormal prressure fluid compartment ) at footwall in southern margin of the basin and uplift sector closely related to faulting should be as a domain or direction for exploration ， and structural traps ( like faulting barrier ， anticline ， etc. ) along with original oil / gas reservoirs at major faulting footwall as the main exploratary targets

    盆地南緣斷裂下盤深層的異常高壓封閉區（流體封存箱） 、與斷裂密切相關的隆起段是今後主要勘探方向與領域，斷裂遮擋、背斜等構造型圈閉? ?主斷裂下盤原生油氣藏是主要的勘探對象。
  9. So it is hope to find gently - biodegradation - oil of pingdiquan formation at declination direction of slope. the paper also points out the next aspect of exploration. east - slope of jimusaer depression and the dropped side of jimusaer rupture are the next advantageous aspect of exploration

    指出吉木薩爾凹陷東斜坡及吉木薩爾斷裂下盤是下一步勘探的有利方向，降解瀝青（或稠油）與巖性共同形成封堵，對油氣富集起封堵作用，在斜坡下傾方向有望發現第二期的受生物降解程度弱的油藏。
  10. Flexion and extension of the joints were normal in 19 cases and mainly normal in 7 cases. lateral crush injuries usually caused transverse rupture in the middle of icl, whereas torsion injuries usually resulted in both ligament rupture and avulsive bone fractures

    側方擠壓傷可造成韌帶中部橫行斷裂;扭轉傷常伴有帶骨塊撕脫;側方擠壓加扭轉傷常致韌帶中部斜形斷裂。
  11. Hengshanbu part have three secondary parts which are tiekesumiao, eastern taole and south of selunkademiao. the zhouzishan part of is charactered by thrust nappe which is composed by faults thrust from west to east, anticlines and synclines, involving much of proterzoic, palozoic and very limited mesozoic in which a suite of conglomerate is found in the front of thrust fractures in late - jurassic

    桌子山段以發育一系列由西向東逆沖的斷裂和背向斜組成的推覆體系為特點，捲入地層多為元古界-古生界，中生界分佈有限，其中晚侏羅世地層在逆沖斷裂前緣普遍見一套礫巖，故推測該段逆沖構造形成於晚侏羅世。
  12. The fracture failure analysis and prevention of front sloping supporting arm

    飛機前支柱斜撐桿支臂斷裂分析及預防
  13. Case study shows that by this approach the imaging profiles with higher quality can be obtained, hence new recognitions of faults are gained, new traps are discovered and good nil shows in slope belt of northern biyang sag have been encountered by drilling

    經實際應用，獲得了較高質量的成像剖面，通過綜合解釋，對泌陽凹陷北部斜坡帶斷裂特徵取得了新認識，發現了一批新圈閉，經鉆探見到了良好的油氣顯示。
  14. In himalayan, the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation. in eastern ore belt, ore - controlling is mainly strike - slip fault and fold ; but in western ore belt, it is block

    喜馬拉雅運動第一期45ma盆地掀斜；第二期23ma以差異隆升剝蝕為主；第三期4ma為脆性變形期，東礦帶近盆邊以走向斷裂及褶皺控礦為主，西礦帶為斷塊控礦。
  15. ( 4 ) through the analysis on the spread of inner structure, thickness change of strata and seismic and geological data in the southern basin of sertengshan - xitieshan, this paper discussed the response of oblique - thrust effect on basin

    （ 4 ）通過對賽什騰? ?錫鐵山南側盆地內部構造展布、盆地內地層厚度變化以及地震地質資料分析，探討了賽什騰? ?錫鐵山斜沖斷裂作用在盆地內的響應。
  16. Bi - material interfacial fracture theories are researched with a phenomenon that cracks extend along interface. a gradient invading model of interface crack at the crack tip can gain stress fields along interface. so a formula of energy release rate for 3d braided cmc is deduced and the corrected formula of the energy release rate is examined with test results

    研究了裂紋沿界面擴展的雙材料界面斷裂理論，利用傾斜侵入界面的裂紋模型解析了裂紋尖端沿著界面的應力場，推導了表徵三維編織cmc復合材料斷裂韌性的能量釋放率公式g _ c ，並且用試驗結果驗證了能量釋放率公式的正確性。
  17. Based on it, favorable exploration areas in wuerxun depression are predicted. the most favorable exploration areas of ktn2 are surennuoer structural zone and huangqimiao structural zone. the more favorable exploration areas are tongbomiao structural zone, wudong slope zone, wuxi fault zone, vvuzhong structural zone and bayantala structural zone. huang yi - l, suwu - 7 and suba - 9 traps ofk1p2 are considered to be the most favorable traps for oil or gas to be drilled

    在綜合上述研究的基礎上，對烏爾遜凹陷南二段的有利勘探區進行了預測，指出蘇仁諾爾斷裂構造帶、黃旗廟斷裂構造帶南部為有利勘探區，銅缽廟構造帶、烏東斜坡帶、烏西斷裂帶、烏中構造帶和巴彥塔拉構造帶為較有利勘探區，南二段黃? - 1 、蘇五- 7 、蘇八- 9圈閉是烏爾遜凹陷南二段油氣下一步勘探的有利靶區。
  18. Throughout researching it has been found that three main types of copper deposits, which mafic - ultramafic rock, marine volcanic rock and porphyry, with middle proterozoic, paleozoic and mesozoic in gansu, china. the cu - bearing formation, deep major faults and late structural - magmatic zones formed in specific geotectonic setting are main ore - controlling and metallogenic factors for copper, gold and polymetallic minerals in this area, and their convergent positions are effective ones formed ore bodies in space

    通過研究認為：鎂鐵質-超鎂鐵質巖型、海相火山巖型及斑巖型三種銅礦類型，是甘肅的主要銅成礦類型，其主成礦階段為中元古代、古生代以及中生代；特定大地構造背景下形成的含礦建造、區域性深大斷裂以及後期斜向構造-巖漿活動帶，是該區銅、金及多金屬成礦的主要控礦因素，三者在空間上的復合是礦床體形成的有利部位。
  19. Since the fault zone had been activated in the later paleozoic, it controlled the evolution of magmatism and metallization belt in taihang mountains. our field workspace is in the northern part of taihang mountains, which is the diagonal area of two main faults

    太行山北段是紫荊關斷裂帶兩主斷裂斜列重疊部位，通過對該區作詳細的野外斷裂構造剖面觀測，比較詳盡地收集了斷裂帶構造組合資料及構造巖標本。
  20. The main steps of the rectification - joining method for broken tube piles were as follows : to rectifying sloping piles, closing cracks, concrete filling and quality testing, with some ways to deal with the problems during practical manipulation

    處理傾斜斷裂的管樁的糾直接樁法的主要實施步驟可總結為斜樁糾直、縫隙閉合、填芯補強和質量檢驗，並得出在具體操作過程中各種問題的解決辦法。
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