fold fault 中文意思是什麼

fold fault 解釋
褶皺斷層
  • fold : n 1 折，折疊。2 褶痕，褶層，褶頁。3 （蛇，蠅等的）一卷，一團。4 （起伏地的）凹處，窪；〈pl 〉（地...
  • 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...
  1. Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin, northeastern yingen - ejinaqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate, tarim plate and kazakstan plate

    查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元。其基底為古生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位的陸緣或島弧褶皺帶，具有古生代造山帶的性質。
  2. They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill. we mark off five kinds of buried hill belts. they include three different kinds of trap on the basis of the cause of trap formation

    本次研究在重新認識濟陽坳陷區域構造背景的基礎上，將濟陽坳陷古生界潛山的形成過程分為四個階段，即古生代早中生代?穩定沉降?隆升?輕微褶皺變形及逆斷層發育階段、中生代?初步斷陷階段?塊斷期、新生代早期?斷拗階段?塊斷潛山形成期以及新生代晚期?坳陷階段?潛山定型期。
  3. There are five kinds of fault - fold assemblage styles which are respectively thrust - nappe structures, imbricate thrust - propagation folds, face to face thrusts, back to back thrusts and positive flower structures

    主要的斷層?褶皺組合樣式有沖斷推覆構造、疊瓦沖斷層?斷展褶皺組合、對沖斷層?沖凹構造、背沖斷層?沖起構造和正花狀構造。
  4. Sequence stratigraphy and lithofacies paleogeography in ziniquanzi formation in piedmont fault - fold belt, southern margin of junggar basin

    準南山前斷褶帶紫泥泉子組層序地層及巖相古地理
  5. Thermal deposits mainly formed during middle - late yanshanian age, related to extension structure, with main mineralization in qingfeng competent deformation zone, western shennongjia fault arch, northern huangling fault arch, xianfeng anticline of enshi platforman fold bundle

    熱液型鉛鋅礦床主要形成燕山中晚期，與滑脫拆離構造密切相關，礦化主要集中於青峰強變形帶、神農架斷穹西部、黃陵斷穹北部、恩施褶皺束咸豐背斜、長陽褶皺束走馬坪背斜中。
  6. According to the spread of nappe and relation between the nappe and depression, oblique - thrust fault zone was divided into three parts in this paper : sertengshan, lvliangshan and xitieshan. ( 3 ) according to macroscopic characteristics of fault zone, cleavage characters of fault zone, drag folds, the reverse " s " fold in the footwall, positive flower structures and small left strike - slip fault, the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section, left - slip fault in plane and the strike - slip displacement increasing from the west to the east

    （ 3 ）根據斷裂斷裂帶的宏觀特徵、斷層帶劈理特徵、斷裂帶附近的牽引褶皺和斷層下盤的平面反「 s 」型褶皺以及斷層上盤剖面正花狀構造和平面左行小型平移斷層，認為賽什騰-錫鐵山斷裂帶運動學主要表現為剖面上的逆沖、平面上的左行走滑特點，並且走滑量具有自西向東增大之勢。
  7. According to the synthetically study of remnant stratum list, sediment system. character of sediment filling, comeback of archetypal basin and feature of tectonic deformation, santanghu basin passed through four formation and evolution phases : ( 1 ) formation and evolution of basin ' s basement ; ( 2 ) formation and evolution of fault - fold to depression basin in permian ; ( 3 ) formation and evolution of depression basin in triassic - jurassic - cretaceous ; (

    依據三塘湖盆地殘餘地層序列、沉積體系、沉積充填特徵和原型盆地恢復，以及不同構造層的構造變形特徵的綜合研究分析，認為三塘湖盆地經歷了如下四個發展演化階段：前二疊紀盆地基底發展演化階段；二疊紀斷陷-拗陷盆地發展演化階段； ：三疊-侏羅-白堊紀拗陷盆地發展演化階段；第三-第四系新生代盆地發展演化階段。
  8. They are dimorphism hill trap > fold hill trap and fault block hill trap. we mark off the hill kinds in term of the cause of hill formation in this research. they are dimorphism hilk fold hill and fault block hill

    總結山五種不同類型的潛山帶，在這五種不同類型的潛山帶上按其成因，主要分為三種類型的圈閉?風化殘丘山圈閉、拱張褶皺山圈閉利斷裂塊斷山圈閉。
  9. 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。
  10. According to the structure characteristics, on the view of 3d modeling, layered rock - mass was divided into three basic types of structure element : continuous rock - mass ( non - folded ), fault rock - mass ( non - folded ) and fold rock - mass

    根據巖體的結構特徵，從三維構模的角度上，將層狀巖體劃分成連續型非褶皺巖體、斷裂型非褶皺巖體與褶皺型巖體3種基本類型的結構單元。
  11. Results obtained in the research are : l. by the virtue of palaeostructure analysis and method of balanced cross sections, we have studied the formation and development history of qianmiqiao buried hills, and indicate that the formation of ordovician buried hills can be mainly divided into four periods, namely, stable uplift period, fold - thrust period, block - fault tilting period, and thermal subsidence and depression period

    論文取得以下成果： 1採用古構造分析和平衡剖面技術，研究了千米橋潛山的形成演化史，指出其下古生界奧陶系潛山的形成主要經歷了穩定抬升、褶皺沖斷、塊斷翹傾和熱沉降坳陷四個時期。
  12. 7. it is indicated the prospects for exploration are beidagang bueried - hill - drape - lik fold oil accumulation belt, baidong structure belt and chengbei fault step oil accumulation belt, which directs the explorations of neogene in qikou depression

    7 、指出了有利的勘探區帶是北大港潛山?披覆背斜油氣聚集帶、白東構造帶和埕北斷階式油氣聚集帶，為歧口凹陷上第三系的勘探明確了實施方向。
  13. The direction of migration was in east and northeast. ( 3 ) this paper introduced the balanced section into the early reservoir description in the sidaogou structure for the first time, and gave a new viewpoint that the sidaogou structure was a fault - bend fold formed by two step thrust fault. the structural stress direction came from the northeast of the hami depression

    首次將平衡剖面技術引入了四道溝構造早期油藏描述的構造研究之中，並首次提出四道溝構造是?至少由兩個階梯狀斷層組成的后傾雙重構造疊加的斷層轉折褶皺，構造應力方向應大致源於北東方向。
  14. 3 ) according to the dayi conglomerate " s gravel composition and direction when water flowed during geological age, comeback the paleogeograph of the longmenshan foreland basin, speculates that the dayi conglomerate " material source is located in the songpan - ganzi fold belt to the east, the pengguan fault to the west of the western sichuan plateau region

    3 ）根據大邑礫巖礫石成分及古流向分析，推測大邑礫巖物源區為松潘-甘孜褶皺帶以東、彭灌斷裂以西的龍門山地區，並恢復大邑礫巖沉積時期巖相古地理，認為大邑礫巖物源主要來自龍門山沖斷帶一側。
  15. There are coherent between the spread of oblique - thrusting structure, fold and fault structure. there were close relationships between oblique - thrust structure and the reverse " s " structure in the basin. both of them are result of the left oblique - thrusting

    逆沖推覆構造呈斜列式形展布與盆地內的也呈斜列式反「 s 」形展布的構造具有密切關系，都屬于斷裂左行斜沖的產物。
  16. Structural characteristics of inversion structure, fold association style, thrust fault zone upright strata developed belt shown in great profiles were also discussed

    對剖面中反映的構造反轉、褶皺組合樣式、逆沖斷裂帶、直立地層發育帶的構造特徵進行了探討。
  17. Moreover, a series of solution to these difficulties are brought forward : applying the theory of fold related to fault to interpret complex structural belts in piedmont : analyzing the features of the surface and underground seismic reservoir prediction and porosity model construction to predicate effectively the texture and quality of sandbodies ; using structural model to direct the construction of velocity model and process prestack migration imaging of seismic data ; utilizing interval velocity to forecast reservoir pressure : improving the drilling technology for pressure detection and prompt protection of vertical well against incline well

    並針對主要難點提出了解決對策：正確應用斷層相關褶皺理論解釋山前復雜改造、開展地表井下地震儲層與孔隙建模有效預測砂體結構與質量，利用有效構造建模指導速度建模與疊前偏移成像、開展層速度預測地層壓力與鉆井壓力檢測及快速防斜打直配套鉆井技術攻關等。
  18. Fold catastrophe model of mining fault rockburst

    礦井斷層沖擊地壓的折迭突變模型
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