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unconformity

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unconformity n.(pl. -ties)1.不相符；不一致；不相稱；不...

n. (pl. -ties) 1.不相符；不一致；不相稱；不順從。 2.【地質學；地理學】不整合；不整合面。 “accord unconformity“ 中文翻譯：   平行不整合“accordant unconformity“ 中文翻譯：   平行不整合“angle of unconformity“ 中文翻譯：   不整合角“angular unconformity“ 中文翻譯：   角不合性; 角不整合; 角度不整合; 斜交不整合; 鈄文不整合“apparent unconformity“ 中文翻譯：   視不整合“azimuthal unconformity“ 中文翻譯：   向位不整合“basal unconformity“ 中文翻譯：   底部不整合“blended unconformity“ 中文翻譯：   混合不整合; 模糊不整合; 隱晦不整合“blinded unconformity“ 中文翻譯：   盲不整合“breakup unconformity“ 中文翻譯：   裂開不整合“buttress unconformity“ 中文翻譯：   長壁狀不整合“chemical unconformity“ 中文翻譯：   化學不整合; 化學分析確定的地層不整合“clino unconformity“ 中文翻譯：   斜交不整合“composite unconformity“ 中文翻譯：   復不整合; 復合不整合“concealed unconformity“ 中文翻譯：   隱蔽不整合“contemporaneous unconformity“ 中文翻譯：   同生不整合“continental unconformity“ 中文翻譯：   大陸不整合“depositional unconformity“ 中文翻譯：   沉積不整合“dispersed unconformity“ 中文翻譯：   分散不整合“divergent unconformity“ 中文翻譯：   成角不整合; 角度不整合“drape unconformity“ 中文翻譯：   披蓋不整合“epeirogenetic unconformity“ 中文翻譯：   假整合“epeirogenic unconformity“ 中文翻譯：   假整合; 造陸不整合“erosion unconformity“ 中文翻譯：   侵蝕不整合“unconformity (= unconformability)“ 中文翻譯：   非整合性“unconformable stratification“ 中文翻譯：   不整合層理

uncongeal

On the base of fully utilizing the available data about tectonic maps and structural elements , the present paper has made synthesized research that used the ways of stratigraphic sequence edge unconformity analysis and stratigraphic thickness correlation analysis , and combined seismic - data interpretation , review of paleo - structure and ancient landform and research of tectonic evolution and petroleum system , and combined region and location , plane and profile and time and spatial . by the synthesis analysis on tectonic evolution of hetian paleo - uplift in tarim basin , the results indicate that : ( 1 ) hetian paleo - uplift is a sedimental and erosional paleo - uplift . the formation and evolution of the hetian paleo - uplift experienced three stages , that is , the uplifting and eroding stage of the caledonian period , the depositional stage of the hercynian period and the destroying stage of the himalayan period , and evolved from paleo - lift to inclining strap at last 本文采用地質和地球物理相結合的研究思路，運用多種技術手段和方法；在充分利用已有構造圖資料和構造要素資料的基礎上，運用地層層序邊界不整合分析法、地層厚度對比分析法，結合地震資料的精細解釋、古構造和古地貌的恢復、構造演化史研究、含油氣系統的研究，和區域和局部、平面和剖面、時間和空間的結合研究，對塔里木盆地和田古隆起構造演化及油氣關系進行了綜合分析，認為： ( 1 )和田古隆起為一沉積?剝蝕性古隆起；形成于志留-泥盆紀；其構造演化可分為三個階段，即加里東期的抬升剝蝕階段、海西期的沉積階段和喜山期的破壞階段，最終由古隆起演變為一斜坡帶。

Through setting up five kinds of most basic geological model and opposite angle unconformity mode , the method of applying 2 - d numerical dissection to 3 - d geological body is discussed in detail , setting up the working method and thoughts from model buildup to the whole process of quantification of geological body and hydrocarbon reservoir 本文通過對5種最基本的地質模型的建立及對角度不整合模式的剖分，詳細探討了對三維地質體進行二維(剖面)數值剖分的算法，建立起地質體和油氣儲層從建模到量化全過程的工作方法和思路。

Guided with the theories of plate tectonics and complex hydrocarbon system , based on the analysis of geological factors of hydrocarbon pools in the northern area of tarim basin , the author puts forward the geological background favorable for and the possible areas most suitable for the formation of complex traps . the identification and description of complex traps lead to the recognization of five large and four middle or small complex traps , by the means of the main techniques and methods include the detailed interpretation of seismic profiles , drilling , logging , map compiling based on the depth of sealing surface and on the superimposed relation of stratigraphic lithology over and beneath the unconformity surfaces , and the the use of the reversion of jason and 3d coherent data . at the same time , the major controlling factors of complex trap oil pool have been analyzed based on the case study of typical oil pools in the paper 目前，復合圈閉勘探及研究工作在我國還比較薄弱，本文以板塊構造學、復式含油氣系統等理論為指導，通過對塔北地區石油地質特征的整體解剖，從動態的角度，綜合分析和探索了塔北地區復合圈閉形成的地質背景及發育的有利區帶和領域，根據鉆、測井及地震剖面精細解釋成果，采用封閉面編圖、不整合面頂底板地層巖性疊置關系編圖方法和jason及三維相干數據體等地球物理反演技術，發現大型復合圈閉顯示2個，中小型復合圈閉4個，復查落實大型復合圈閉3個，并通過典型油氣藏解剖，分析了塔北地區復合圈閉成藏主控因素分析。

The topic of this paper is structure , firstly analyse the earth structure setting of tarim basin and tectonic evolution of tazhong area in silurian - devonian , and give silurian - devonian stratum control and effect , then study the relationship of the development of tazhong uplift , fracture unconformity igneous rock and and oil - gas , at last , on the base of the analyse about history of reservoirs formation , forecast reservoirs pattern , point out favored oil and gas bearing structure and the target . and obtain some important conclusion . 1 本文以構造研究為主題，詳細的分析了塔里木盆地志留泥盆系沉積時的大地構造背景和塔中地區的構造發展，以及它們對研究區志留?泥盆系地層的控制和影響，同時在研究了塔中隆起的形成發展演化、斷裂、不整合以及火成巖等構造特征的基礎上，分析了它們與油氣的關系，結合志留泥盆系突破井的成藏史分析，預測了成藏模式，最后指出有利含油氣構造，并進行了簡單的目標預測。

The features of these sequences arerbefore sequence i deposited during the rapid subsidence of the depression , the range of the sediment is limited . sequence ii is the first series of source and reservoir rocks of the depression . there are regional unconformity at the bottom of the sequence iii . the rock type are variety . this sequence is evaluated as good source rock , sequence iv is associated with the first section of duhongmu formation , thick mudstone at the bottom and the thick single sandston are the main rock type . this sequence are evaluated as good source rock and reservoir . sequence v associated with the second and the third section of duhongmu . which is mainly mudstone and can be regional capping rocks 層序對應于阿爾善組二段，為深色泥巖與砂礫巖不等厚互層，是本區的第一套烴源巖和儲集層，可以作為本區儲層。層序對應騰格爾組，此時凹陷擴張，沉積層底部具有區域性的沖刷面，巖性變化大，是較好的生油層。層序對應都紅木組一段，下部泥巖發育，單砂層較厚，是主要的生油層和儲層。

Tncyclic diterpanes c20 , c21 and c23 distribution also has relationship with oil gravity , oil and gas production , as well as oil pool formation timing and oil source . rising - patterned oil originates from fengcheng formation , while peak - patterned oil from xiawuerhe formation . four types of migration and accumulation models are put forward : ( l ) fault controlled migration and accumulation along ridge far from source region ; ( 2 ) fault and unconformity controlled migration and accumulation around source region ; ( 3 ) fault controlled migration and accumulation in the slopes within source region ; ( 4 ) biogenetic and low temperature catalyzed gas migration and accumulation in middle and shallow formation 受擠壓背景控制，研究區內海西期形成的斷裂，全部為逆斷裂，活動期長，可以延續到印支期和燕山期，斷開層位可以從石炭系上延至誅羅系，它們對區域構造、沉積、油氣運聚有顯著的控制作用；而燕山期形成的斷裂多為小型正斷裂，部分為株羅系和白要系內部斷裂，部分從徐羅系斷至白圣系。

The basin has three evolutionary stages including intracontinental rift basin in p1 - p2 , down basin in t2 + 3 - k and the strong trust - orogeny process in n - q . according to the unconformity contact relationship and sedimentary components , santanghu basin is divided into four tectonic sequence such as : o - c tectonic sequence of basement , pi - p3 tectonic sequence , t - k tectonic sequence and n - q tectonic sequence 根據盆地地層之間的不整合接觸關系，考慮到各層序沉積物組成與生物組合特征等因素，將三塘湖盆地劃分為： ( o ? c )基底構造層序，二疊系( p )構造層序，三疊系( t ) ?白堊系( k )構造層序和第三系、第四系構造層序。

However , the authors discovered recently that the top and bottom surfaces of the loushanguan formation are palaeokarst unconformity interfaces , and there are a lot of interbeds of granular ( oolite , pisolite and oncolite ) dolomite and algae - mat dolomite , especially sedimentary structures such as the bird ? s eye , stromatolite , cross bedding and tepee structures 但筆者新近研究發現，其頂、底均為古巖溶不整合面，并有大量顆粒(鮞、豆、核形石)白云巖和藻紋層白云巖夾層，還有許多鳥眼構造、疊層石構造、交錯層理、帳蓬構造存在。

There are a variety of causes that may bring up uncomfortable usage , traffic jam , even malfunction of glass lifer , such as bad stamping part of doors , bad tolerance with inner / outer watertight seal and dimension and material of window guide - slot , problems with regulator itself , as well as unconformity of window glass application and its design specification 引起車門玻璃升降器失效的原因很多，其中車門沖壓件不規范，車門內外玻璃擋水膠條及玻璃導槽的尺寸形狀及材質存在偏差，車門玻璃升降器本身存在問題，以及車門玻璃與設計要求不符等等都是導致車門玻璃升降不暢，卡滯，甚至失效的重要原因。

Kongxi buried hill shows following features in the seismic profiles : the structures are asymmetric . there is flexural syncline on the east side and a monocline on the west side . asymmetric repetition of stratigraphic units is present in the drill wells and the dips of beds and faults are gentle . the permo - carboniferous system of both sides almost lie in the same slope and the events of cambrian or upper proterozoic are continuous from east to west . the phenomenas suggest that kongxi buried hill could be a thrust belt been traced which consists of reverse faults . the imbricate faults mainly effect pre - jurassic strata . there are obvious angular unconformity between jurassic - cretaceous system and paleozoic involved deformation of thrust . the thrust front in some place has cut off the beds of jurassic - cretaceous system . the structural style of the thrust structure changes along the strike of the kongxi buried hill 地震和鉆井資料揭露的孔西構造帶前第三系潛山的地質特征可以歸納為：構造帶總體上不對稱構造帶內部有地層重復現象石炭二疊系地層的位置明顯高于兩側的同一地層的高度。用由34條向東傾斜的逆沖斷層組成的疊瓦扇構造模式能夠比較合理地解釋上述地質特征。該帶向東傾斜的逆沖疊瓦狀斷層組主要影響前侏羅系地層，侏羅白堊系與卷入逆沖構造變形的古生界地層之間有明顯的角度不整合。

On the basis of comprehensive analyses on hydrocarbon accumulation conditions in the four representative foreland basins , kuqa basin , southern junggar basin , western sichuan basin and northern margin of qaidam basin , some conclusions are made as follows ; the foreland basins in central and western regions of china are characterized by multi - set source rocks dominated by coal measure ; heterogeneous reservoirs ; multiple and sealing cap nick ; anticline traps ; unblocked transport system composed of fault , unconformity and highly permeable sand body ; anti poor conservative conditions . etc 在綜合分析和對比庫車、準南、柴北緣和川西等具有代表性的前陸盆地的油氣成藏條件的基礎上指出，中西部前陸盆地具有以煤系為主的多套源巖，發育非均質儲集層，多套多封閉性的蓋層，以背料為主要圈閉；斷裂、不整合和高滲透砂體組成良好輸導體系，保存條件較差等特點。

The stratums containing mine , tectonic - hydro thermally process , magma activity , alteration react to district mineralization in degrees . the belt of granite facies , the inside and outside contact belt of rock body , the joining belt of tectonic - hydro thermally superimposed , the stratum belt of unconformity contact are the main enrichment belt 含礦地層及礦源層、構造-熱液作用、巖漿活動、變質作用都在不同程度上對區域成礦起作用，而花崗巖相變化帶、巖體內外接觸帶、構造?熱液疊加交匯帶、地層不整合接觸帶則為金礦化主要富集帶。

The good reservoir facies are braided stream and braided delta in alaer area , fan - delta in arhati area and lake - floor fan in shizigou - ganchaigou area . all of these areas are the main targets for oil exploration , it has discovered that there is an important unconformity between upper youshashan and lower youshashan formation of tertiary , on which there are a large amount of erosion and long time of depositional hiatues 在上述研究的基礎上，對區內油氣勘探的有利區帶進行了預測，指出阿拉爾北東辮狀河三角洲相帶、阿哈提南東扇三角洲相帶和獅子溝一干柴溝湖底扇相帶為區內有利的儲集相帶，是今后勘探的主要目標。

( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian , late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic . structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave . most traps in the area formed or typed at last in the himalayan episode , dispersed on the north and south belts ( 4 )研究區構造與地層不整合圈閉的形成和發育受志留-泥盆紀、晚二疊世-第三紀、漸新世-第四紀三個擠壓階段的控制；早古生代主要發育非構造圈閉和復合圈閉，晚古生代和新生代則主要發育構造圈閉：構造圈閉主要發育在南北兩帶上，其次為中帶；非構造圈閉主要發育在和田凹陷以北的地區；研究區內大多數圈閉是喜山期形成或最終定型的，在南北兩帶都有分布，而海西期圈閉主要分布于研究區中帶瑪南構造帶處。

4 . the types of of oil & gas are systematicly summarized . there are three basic type : first : lateral migration along layers with medium distance formed self - producing oil reservoir of neogene . second : migration along fault with short distance formed shallow oil reservoir . third : lateral migration along interlayer and unconformity with long distance 4 、系統總結了歧口凹陷油氣二次運移的三種基本方式：一是中距離沿層側向運移形成下第三系原生油藏；二是短距離沿斷裂通道運移，形成淺層油藏；三是長距離沿層間或不整合面的側向運移。

Their distribution of deposition control lithology subtle trap , die - out around paleo - uplift the distribution of subtle traps in the slope , subtle trap forms along faults and above and beneath unconformity boundary . through exploring and studying in huanghua depression many years , we gradually summarize a series of methods and technologies for subtle trap exploration , they are precise stratigraphy correlation on the basis of sequence stratigraphy , including micromarker correlation , element logging , high frequent cycle stratigraphy and precise sequence stratigraphy , besides conventional biography stratigraphy , logging correlation . through using facies analysis method , the type and distribution of reservoir are determined 在黃驊坳陷通過多年的摸索和引用，逐漸形成了一套系統的隱蔽油氣藏的研究方法和技術，它們是以層序地層學為代表的地層精細劃分方法，用來解決地層劃分及歸屬問題，除常規的生物地層學、巖電特征對比方法外，創新性的運用了包括微標志層劃分方法、元素測井方法、高頻旋回對比方法及精細層序地層劃分方法等四種精細地層劃分方法。

Complex subtle trap further falls into structural lithology , structural unconformity and lithology unconformity reservoirs . so far , the main theories to study subtle trap include early seismic stratigraphy and late sequence stratigraphy , between them sequence stratigraphy is most effective , its stand tract concepts for different depositional systems is of important significance 目前，世界上研究隱蔽油氣藏的理論主要有早期的地震地層學理論及新興的層序地層學理論，其中層序地層學理論最為引人注目，且是尋找隱蔽油氣藏的最好的方法，其不同水位期對不同沉積體的尋找具有指導意義。

The sanwan opeirogeny is marked by the regional disconformity - angular overlapping unconformity below the upper triassic sanqiutian and yangmeilong formations , while the sandu opeirogeny is recorded by the regional disconformity - angular overlapping unconformity below the upper triassic zaoshang , duojiang and tanglong formations 三灣造陸運動以上三疊統三丘田組、楊梅垅組之下的區域性假整合-角度超覆不整合為標志；三都造陸運動以上三疊統造上組、多江組、唐垅組之下的區域性假整合-角度超覆不整合為特征。

The formation and alteration of uplifts and depressions resulted in the complex stratigraphic architecture and unconformity configuration , which significantly constrained the formation and distribution of stratigraphic or structural - stratigraphic traps in the large superimposed basins in the western china 中國西部大型疊合盆地內古隆起的形成演化和隆、坳格局的變遷可導致復雜的層序結構和不整合分布樣式，對地層或構造地層圈閉的形成分布具有重要的控制作用。