thrust fault 中文意思是什麼

thrust fault 解釋
逆沖斷層
  • thrust : vt (thrust)1 猛推,沖;猛撳,沖入,插入,推入(出),突出,伸出,塞,刺,戳,戳穿。2 逼迫,把[...
  • 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. 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。
  2. 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。
  3. Muir wood r., 1984. problems of estimating earthquake recurrence from geological investigation in thrust fault terrains. proc. int. comp. on seismic microzonation, ech - cheliff algerea. 1, 147 - 159

    國家地震局地質研究所, 1994 .廣東第三核電廠沙環廠址設計基準地面運動確定
  4. 2. it is the first time to divide the structure of qianmiqiao buried hills into three structural layers : buried hills thrust fault block, paleogeomorphic relict mountain and lowland, tilting horst block

    2首次將千米橋潛山構造劃分為三層結構:即潛山內幕逆沖斷塊、古地貌殘山與低地和翹傾地壘塊。
  5. The basin - formed mechanism, evolution model and petroliferous geological features of compresso - shear basins in the world are analyzed, by which six aspects of the features are summarized as follows : 1 ) in the compresso - shear process, the sedimentary speed of basin is high, forming thicker coarse - grained clastic rocks which normally shape good petroleum reservoir ; 2 ) the source rocks of basin tend to coming from the organic matter - enriched rocks formed in pre - compresso - shear stages, except that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in pre - compresso - shear stages, e4xcept that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in frontal of deep depression ( fore deep ) of thrust belt ; 3 ) the en echelon folds ( including anticline and fault - nose structure ) are generally as good oil traps ; 4 ) the compresso - shear process is helpful to hydrocarbon accumulation ; 5 ) it may promote the maturity and hydrocarbon - generating process of organic matte, and 6 ) the thrust belts in the surrounding areas of compresso - shear basin are favorable are favorable domains for petroleum concentration

    摘要通過對世界上壓扭性盆地的成盆機制、演化模式和油氣地質特點分析,總結壓扭性盆地具有6個方面的石油地質特徵:壓扭作用期間盆地的沉積速率較高,一般形成較厚的粗碎屑沉積,它們常構成很好的油氣儲集層:盆地的烴源巖往住來自於前壓扭期砂成的富含有機質的巖石,但在強烈的壓扭作用期間,在沖斷帶的前緣深坳陷(前淵)中有可能發育深水半深水相的烴源巖;壓扭(張扭)作用期間形成的雁行式褶皺(包括背斜和斷鼻等)往住是很好的油氣圈閉;壓扭作用易於成藏;壓扭作用可以促進有機質的成熟生烴作用;壓扭性盆地的周邊沖斷帶是油氣賦存的有利部位。
  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. 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。
  8. We obtained the uniform data distribution from discrete data points by inserting spatial dots and then set up digital elevation model ( dem ) of correlative area through constructing mutual linked triangle net. the isoline graph was implemented based on this model. during the processes, we combined the technology of stratification computing when inserting special dots in fault area with the technology of stratification triangle net in fault area for dealing with thrust data

    然後介紹了在本研究中構造逆斷層地質等值線的基本思路:從離散數據點結構出發,採用空間數據內插方法進行數據的均勻化,通過三角剖分構造出相互連接的三角形網路結構來建立起相關區域內的數字高程模型,利用該模型構造出相應的地質等值線圖,其中使用擴展點與斷層區的關系屬性進行斷層區分層空間插值計算處理和斷層區域的分層三角形網格化處理相結合的技術,實現逆斷層數據的處理和等值線繪制。
  9. 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。
  10. The ne - strike compressional faults are not intersected with the ew ma in fault zone, but a kind of transform structure resulted from its right lateral strike slip, and one of the typical example is the mesozoic thrust systerm in the northeast side of the main fault in western liaoning

    在青龍斷裂帶兩側,分佈有許多北東向壓性斷層,它們與東西向主斷裂帶不是簡單的切割關系,而是東西向主斷裂帶右行走滑活動中的分支斷裂,位於青龍斷裂帶北東側的遼西地區中生代逆沖推覆構造,也是青龍斷裂帶在右行走滑作用下,因構造方向的改變發生構造轉換的結果。
  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. 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。
  13. After current data analysis and field investigation, the authors consider that the xiangfan - guangji fault is a composite fault belt making up of various subgrade faults of different ages, including the early - stage ( indosinian - yanshanian ) southward thrust and late - stage ( himalayan ) northward thrust

    摘要本文在系統總結現有資料的基礎上,運用板塊構造理論和現代造山帶研究方法,通過野外工作,指出襄樊~廣濟斷裂(帶)是由多條不同時期斷裂組成的復合斷裂帶,它包括早期(印支~燕山期)由北向南的逆沖構造和晚期(喜馬拉雅期)由南向北的逆沖推構造。
  14. 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。
  15. 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。
  16. The present longmenshan foreland basin lies between the longmenshan thrust belt and the longquanshan fault. the dayi conglomerate at the bottom of the chengdu basin, although people of the past having studied a certain degree, hasn " t same sugest

    大邑礫巖的地質時限為上新世-早更新世,時代界定在4 . 6ma - 0 . 82ma之間,顯示該區第三紀與第四紀之間是連續沉積的,其間不存在構造事件。
  17. 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。
  18. Bedding - plane thrust fault

    順層沖斷層
  19. The main thrust of this study are follows : the primary study provides in detail the area structural properties including the fault systems, structure units, and trap types ; the secondary study including the sedimentary systems including stratigraphic classifications, depositional environment properties, infilling - evolution properties, and oil source analysis ; the third area of study including the geologic property of the north slope zone ; and the final area of study provides an analysis of gas and oil accumulation, the types and distribution of reservoirs, and the pool - forming models used

    本研究主要從事了以下工作,較為詳細地研究了該地區斷裂體系、構造單元、圈閉類型等構造特徵;從地層劃分、沉積特徵、沉積環境、充填演化特徵、油源分析等方面研究了該地區的沉積體系;詳細地研究了油氣資源豐富的北部緩坡階梯帶的地質特徵;根據成藏動力學系統理論,較為詳細地研究了該區的油氣運聚模式、油氣藏類型及油氣藏分佈規律。
  20. This paper discussed thrust fault - tolerant control technology for zhishui auv, designed at harbin engineering university

    本文主要以哈爾濱工程大學研製的「智水」型水下機器人為對象,探討水下機器人推力器容錯控制技術。
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