stratigraphic analysis 中文意思是什麼
stratigraphic analysis
解釋
地層分析- stratigraphic : adj. 【地質學；地理學】地層學的。adv. -cally
- analysis : n. （pl. -ses ）1. 分解，分析；【數學】解析。2. 梗概，要略。3. 〈美國〉用精神分析法治療（＝ psychoanalysis）。
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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。 -
The stratigraphic sequences and sedimentological characteristics indicate that the main body of the bayan har basin is composed of triassic flysch sediments deposited in a foreland basin during the triassic. in the study of jinshajiang orogenic belt, in the applying archipelago theory and particular anatomies to basin analysis in this orogeny, the model of jinshajiang archipelago mountain building and basin building is set up. the orogenic - sedimentology and sedimentary basin analysis system is printed archipelago paleogeography any more
在金沙江造山帶研究中，將多島弧盆理論應用於這個造山帶的沉積盆地分析研究中，對金沙江多島弧盆造山帶進行了詳細解剖，建立金沙江多島弧盆系造山造盆的模式，進一步發展造山帶沉積學和沉積盆地分析理論體系。 -
After have systematically studied sequence stratigraphy of chagan depression, a analysis method of high precision sequence stratigraphic framework in fault - depressed lacustrine basin. the core of the establishing framework is exploration - significant identify of sequence, division of 2, 3, 4, 5 grades sequence and analysis of base - level based on lithologic log or well - logging, high - resolution seismic inversion constrained to well data. then using the results of 2d seismic data, and interpret sequence to enhance the precision of interpretation
斷陷盆地高精度層序地層格架建立的核心是用鉆/測井和井約束條件下的高解析度儲層橫向預測剖面等高解析度資料進行具有勘探意義的二、三、四和五級層序的界面識別、層序劃分和基準面變化分析，在此基礎上標定常規地震剖面，進行區域層序地層分析，達到提高層序地層解釋精度的目的。 -
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徵的整體解剖，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，採用封閉面編圖、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，並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。 -
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
本文採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；形成於志留-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。 -
The seismic stratigraphic analysis of taowan conglomerate in luonan, shaanxi
陜西洛南陶灣礫巖地震機理新認識 -
Basing on the analysis and correlation of the7 wells, 8 seismic sequence boundaries are obtained by logging - seismic correlation, based on seismogram synthesis. more over, they can be traced in the studying region. the synchronic sequence stratigraphic framework is established finally
在單井分析和連井對比的基礎上，通過合成記錄標定、地震層序的分析，識別出8個三級層序界面，而且完成了全區的主幹剖面解釋，建立了井震統一的等時層序地層格架。 -
On the basis of all kinds of stratigraphic and petrologic data of outcrop and well sections, the maps of single factors and sedimentary facies of the paleocene - eocene, oligocene and miocene were compiled with the single factor analysis and multifactor comprehensive mapping method proposed by professor feng zengzhao
摘要根據柴達木盆地北緣露頭剖面、鉆井剖面的地層學和巖石學研究所取得的各種定量及定性資料，採用馮增昭教授倡導的單因素分析多因素綜合作圖法，編制了柴達木盆地北緣結綠素紅山地區古新統始新統、漸新統和中新統的各種單因素圖和沉積相圖。 -
The paper analyzes the reasons why these lakes disappeared in xiaoqinghe river drainage by historical documents, analysis of stratigraphic profiles and research of place names
通過查閱歷史文獻、地層剖面分析、地名?證等多種途逕和方法對小清河流域的湖泊消失的原因進行了研究和分析。 -
Analysis of known volcanic rock reservoirs indicate that they exist in the following two types : one is volcanic rock lithofacies, the other is the stratigraphic or fault - stratigraphic
根據對已知火山巖油氣藏的解剖分析，主要存在以下兩種類型：一是火山巖巖相型，二是地層或斷層?地層型。 -
And it is also possible to analyze the reservoir property in reservoir framework. taking the reservoir of zonation 6 - 10 in s32 of pucheng oil field in henan province as an example, we founded the detailed reservoir stratigraphic framework through base - level correlation. in the strata frame, sediment distribution and its development are discussed based on sediment volume partitioning and facies differentiation analysis
依據基準面變化中的過程?沉積響應，分析沉積過程中沉積物體積分配及與其相伴生的相分異，進行等時地層對比，建立精細地層格架，預測儲層空間展布及其非均質性的思路為儲層精細描述提供了新的方向。 -
From connecting - well profiles that reflect filling characteristic of basin, combining with comprehensive analysis of seismic stratigraphic framework, the sequence stratigraphic framework of tertiary was established in hong - shi area and the distribution of sedimentary systems in time and space was deeply discussed
通過能揭示區內第三系沉積充填特徵的連井剖面，結合地震層序地層格架的綜合分析，建立起了紅獅地區第三系的層序地層格架，探討了沉積層序的時空分佈規律。 -
A sequence stratigraphic analysis of the jurassic coal measures in yuqia region of northern qaidam basin
柴北緣魚卡地區侏羅紀含煤地層層序地層學研究 -
High resolution sequence stratigraphic analysis of sandstone reservoir in mt oilfield
油田砂巖儲層高解析度層序地層分析 -
The methods of the studies involve stratigraphic analysis and cores samples analysis
在此基礎上，綜合評價孔店組儲集砂巖的儲集性能。 -
Application of high resolution sequence stratigraphic analysis in oil sand correlation
百色盆地百49塊百崗組三段高解析度層序地層學分析 -
High - resolution sequence stratigraphic analysis of the delta depositional system of shahejie formation in dongying depression
東營凹陷沙河街組三角洲體系高精度層序地層分析 -
Sequence stratigraphic analysis and sedimentary study on yaojia formation in northern taikang area of northern songliao basin
松遼盆地北部泰康北地區姚家組層序地層分析與沉積相特徵 -
To provide the students with a needed background in modern stratigraphy and a chance to learn the methods of stratigraphic analysis to be used in their future research
奠定修課同學研究所需之地層學基礎，輔助同學練習研究的方法，並為未來之論文研究作一初探。 -
The stratigraphic analysis reveals that the upper part of kongdian formation is characterized by thickness range from 461 - 744 m and average of thickness of 602. 5 m. the number quantity of sandstone increased to the north and northwest, indicating more sand bodied are found at these directions
地層學分析表明南斜坡主要發育孔店組上段，地層自南向北逐漸增厚，地層厚度一般為461 - 744m ，平均厚602 . 5m 。
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