斷層盤 的英文怎麼說
中文拼音 [duàncéngpán]
斷層盤
英文
side of fault-
The results of 2 - d resistivity inversion of the yishui - tangtou and the liujazhuang faults indicate that electrical structures on both sides of the fault zone present obvious difference, the resistivity of the hanging wall is low and partially high, while that of the foot wall is high, and the faults are high - obliquity faults
沂水湯頭斷裂、劉家莊斷裂的二維電阻率反演結果表明,斷裂帶兩側的電性結構呈現出整體性的差異,正斷層的上盤為低阻區和局部高、低阻擾動區;而斷層下盤多為均勻的高阻區;斷層為高角度斷層。The study area is composed of sandstone & conglomerate reservoir of alluvial fan & fan delta, which belong to sha3 lower member and sha4 upper member of lower tertiary of yong " an town oilfield in dongying depression. the target stataum develops in the hanging wall of the synsedimentary fault in the scarp zone of dongying depression. the frequently intense movements result in the variation of sandstone and conglomerate reservoir and the evolution of the time and space of sha3 lower member and sha4 upper member in yong " an town oilfield
研究區是東營凹陷永安鎮油田沙三下段、沙四上段的沖積扇和扇三角洲砂礫巖體,目的層發育在東營凹陷陡坡帶同生斷層的下降盤,因斷層多期強烈活動,導致永安鎮油田沙三下段、沙四上段的砂礫巖體成因類型多,時空演化變化大,在扇根一帶小層對比難度大,給油田開發帶來很大的難題,在這種背景下進行流動單元研究難度更大。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。Near shore sub - aqueous fans, fan delta and delta occurred on the footwall of the hainan marginal fault, whereas turbidity fans developed in the deep water area and the footwall of the hainan no. 2 fault
海南邊界斷層下降盤分別發育近岸水下扇、扇三角洲和三角洲沉積。海南2號斷層下降盤及深水區域濁積扇沉積發育。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。The differentiation and the amalgamation among the nations made the national culture more complex, inducing the national and religious conflicts which were of long history and hard to be resolved
這種民族文化錯綜復雜的狀態,鑄就了南斯拉夫根深蒂固、盤根錯節的民族宗教沖突。由此,文明斷層帶構成南斯拉夫民族問題長期存在的內在文化根源。( 5 ) based on the integrated sequence stratigraphy analysis of typical wells section and many well - to - well section, the control of hinge fault is confirmed. system tracts of downfaulted block perfectly develop, from lower position to higher position, upfaulted block ( west - north region of the gentle slop ) is in turn pgc, tst, hst, overlapping in sb
( 5 )通過典型井剖面及眾多連井剖面的層序地層分析,證實樞紐斷層的控製作用,斷層下降盤各體系域發育完整,而其上升盤(西北斜坡區)由低處向高處,依次是pgc 、 tst 、 hst超復于sb之上。On the basis of composite exploration methods with gravity prospecting electric survey and setsmic prospectlog in mount liupanshan basin, a geophysical joint inversion method is applied to research and solve the problems about the contact relation between the basin and the mountain, distribution of faults and deep target strata, favorable structural trap features, and so on, which will provide a scientific basis for arrangements of oil and gas exploration
摘要在六盤山盆地進行重力、電法和地震綜合勘探的基礎上,應用地球物理聯合反演方法研究和解決盆山接觸關系、斷層分佈、深部目的層分佈和有利構造圈閉特徵等問題,為油氣勘探部署提供科學依據。Through reservoir prediction, it indicated that the reservoir in mainan structure and mopan - laowan buried structure which located in short limb and bottom wall were finely developed, this two areas were the primary area for the further exploration and drill site design in dachiganjing structural belt
通過儲層橫向預測,發現麥南構造和陡翼斷層下盤的磨盤老灣潛伏構造儲層較發育,是大池乾井構造帶下一步勘探及井位部署的重點區域。By means of the method of filtered convolution, we process the nearly 15 years ' ( 1986 - 2000 ) observational data of the cross - fault short level at tianma station of fujian and draw the deformation features of the relative movement of both sides of the fault before mid - strong earthquakes in fujian and the coastal areas
摘要應用褶積濾波的方法對福建天馬跨斷層短水準觀測點近15年( 1986 ~ 2000年)的觀測資料進行了計算、處理和分析,歸納出了福建及其沿海地區中強震發生前該斷層兩盤的相對運動變化特徵。Xianhe block is located in the shallow water area of bohai bay with an area of 100 km2. geologically, it lies on the footwall of hainan no. l fault within liaohe western depression
仙鶴地區位於渤海遼東灣灘海地區,遼河西部凹陷東側海南一號斷層的下降盤,面積約100km ~ 2 。With an area of 100 square kilometers, the xianhe 3d seismic survey is geographically located at the liaodong gulf, bohai sea, and geologically at the down - block of the hainan fl fault, eastern margin of west - depression, liaohe basin
仙鶴地區位於渤海遼東灣灘海地區、遼河西部凹陷東側的海南一號斷層的下降盤,面積約100km ~ 2 。本區目前有兩口探井, lh11 - 1 - 1和時1井。The significance of evaluation of optic disc by heidelberg retinal tomography in primary open - angle glaucoma
海德堡視網膜斷層掃描儀在開角型青光眼視盤檢測中的意義There are four kinds of fault, according to geometric character of fault, which are deep - seated fault, the fault surface cross cap formations but is not reach to ground, the fault surface cross to ground and ground fault. discuss the closure ability, based on the active stage and the lithlogic of two sides in fault
根據斷層幾何學特徵和成因歷史分為四類:深部斷層、斷穿蓋層未至地表斷層、通天斷層及表皮斷層,以其活動時期和斷層二盤巖性特徵為基礎,分類討論了封堵性。The exploration experience of the los angeles basin demonstrates that the footwall fault traps can have very significant reserves
洛杉磯盆地的勘探實踐說明斷層下盤圈閉有時也能含有很可觀的儲量。Therefore, we can conclude from the predictions of reservoirs and pressure in the area that the major exploration prospects should be the reservoirs between the fl and f2 faults and the turbidity fan sandstones in the down - block of f2 fault
F5斷層封堵性能相對較差。從儲層預測和壓力預測結果看,本區沙河街組的勘探重點應該放到中臺階及下臺階二號斷層下盤附近的濁積體發育區。Analysis on distribution features of gas outburst from two walls of normal fault and geological origin
正斷層兩盤的瓦斯突出分佈特徵及其地質成因淺析Seismic inversion results indicate that the delta sandstone reservoirs occurred extensively in the 2nd and 3rd intervals of dongying formation, lower tertiary, and become poor only to the western margin of the survey area. in contrast, the fan delta sandstones in shahejie formation developed mainly in the area between fl and f2 faults, and turbidity sandstones locally in the rest of the survey area
儲層預測結果表明,東二、三段儲層除工區北部西側外,普遍發育較好;而沙河街一、二段和沙三段儲層主要集中在f1斷層下盤的中臺階地區及f2斷層下盤,其它地區發育一些規模不等的濁積扇。The result shows, the poluokenu fault is the borderline for the movement direction of fault, the characteristics of the faults are pull apart in the north part, but in south part the characteristics are convergence
計算表明天山中部地區內部斷裂兩盤的運動方向以婆羅科努斷裂為界,北部各斷層表現為拉張特徵,南部總體表現為聚合特徵。Meanwhile, the function of fault which palyed in the secong migration of oil & gas are discussed and indicated that time of fault movement, combination type of fault and fault movement caused the difference of layer ' s attitude between the two fault walls and face to face lithologic relationship greatly influenced the orientation and scales of oil & gas second - migration
同時對斷層在油氣二次運移中所起作用進行論述並認識到斷裂活動的時間、斷裂的組合樣式、斷裂活動造成兩盤地層產狀的差異和巖性對置關系對油氣二次運移的方向、規模具有重要影響。分享友人