fluvial facies 中文意思是什麼

fluvial facies 解釋
河流相
  • fluvial : adj. 1. 河的，河流的。2. 生在河中的。3. 河流沖刷作用形成的。
  • facies : n. 〈pl. 〉 〈單復同〉1. 顏面，外觀；外表。2. 【生態】演替系列混優種社會，演替系列變群叢。3. 【地質學；地理學】相。4. 【醫學】面色；表面。
  1. Characterization of sedimentology in fluvial facies reservoir

    河流相儲層沉積學表徵
  2. Pollen sedimentary facies of fluvial sediments on north china plain

    華北平原沖積物孢粉沉積相研究
  3. At the end of sq9, sedimentary environment converted to fluvial facies from limnetic facies

    到層序9沉積末期，沉積環境由湖沼相過渡為河流相。
  4. According to the regional geology and the character of the lithofacies and well - logging facies, 4 kinds of sedimentary facies and 3 kinds of depositional system : marine system, delta system and fluvial system have been identified. the sedimentary facies of taiyuan formation is marine faceis, up to sanxi formation, the sedimentary facies is delta facies, the xiashihezi formation hel and he2 member are braided river facies, he3 member is meandering river facies. the mains types of sandstone of taiyuan formation are lithic quartzarenite and quartzarenite ; the mainly types of sandstone of sanxi formation and xiashihezi formation is litharenite

    通過對20餘口井2000多米巖心的觀察和對40幾口井的測井數據解釋、對比，在研究區目的層段識別出了12種基本巖相和9種測井相類型，在區域沉積背景和單井相劃分的基礎上，根據巖相和測井相組合特徵，在太原組?下石盒子組劃分出4種沉積相和若干沉積微相，並進一步劃分為3類沉積體系：濱淺海沉積體系、三角洲沉積體系和河流沉積體系。
  5. From paleocene to miocene, the sedimentary facies evolved from the extensive alluvial fan to the braided fluvial river environment

    從古新世到中新世，柴達木盆地北緣經歷了由大規模沖積扇沉積到辮狀河沉積的演化過程。
  6. The basic principle and method of 3d stochastic modeling of sedimentary microfacies are discussed according to geological and acoustic impedance data of well - logging constrained seismic inversion, and a case study according to stochastic modeling of fluvial facies reservoir of the minghuazhen formation of neocene in a certain block of bohai bay basin is used to show the general process of this research

    摘要探討了綜合應用地質及測井約束地震反演信息進行三維沈積微相隨機建模的基本原理、思路與方法， ?以渤海灣盆地某區塊新近系明化鎮組河流相儲層?例，說明這一研究過程的基本步驟，包括井眼沉積微相解釋、測井約束地震反演、波阻抗與地質相的概率關系分析、隨機模擬方法選擇、地質統計特徵分析、三維隨機建模、隨機模擬預測的多解性評價。
  7. On the basis of previous research works, new exploration wells, new appraisal wells and 3d seismic material are added to new research work in which rock and mineral, sedimentary facies and oil bearing characters are studied deeply by employing the methods of petroleum geology, sedimentary geology and reservoir geology. the results of reservoir prediction on fluvial sandbody in the upper of formation of guantao group obtained by using coherent analysis and acoustical impedance inversion bring good effect to the exploration and development of chengdao oilfield

    本文在以往工作的基礎上，補充新鉆探井、評價井和三維地震資料，運用石油地質學、沉積地質學、儲層地質學等原理方法，對埕島油田主力含油層系館上段地層的巖礦、沉積相及油氣富集特徵進行了深入的研究，對館上段河流相砂體進行了以測井約束地震反演為主的儲層預測研究，研究成果為繼續開展埕島油田的勘探開發提供了重要依據。
  8. Hot event deposits occurred in liantuo formation of lower sinian, interbedded in fluvial facies sandstones and siltstones

    熱事件沉積產物見于下震旦統蓮沱組，夾于河流相沉積的砂巖及粉砂巖中。
  9. Grain - size accumulation percentage of the aeolian sands in the past 150 ka in milanggouwan section is mainly characterized by the aeolian palaeo - mobile dune sands, which are composed of majority fine sands and minority very fine sands. there is n ' t almost any silt and clay. those of the fluvial facies, especially the lacustrine facies and palaeosols, are mainly composed of very fine sands and also contain some quantities of silt and clay

    米浪溝灣剖面150kabp以來風成砂的粒度累積百分含量以古流動砂丘砂物質為主，其中以細砂含量最高，極細砂為次，幾乎不含粉砂與粘土；河流相、特別是湖沼相與古土壤以極細砂含量占優勢，且具一定含量的粉砂和粘土。
  10. Dividing the sedimentary facies as a delta - lacustrine facies according to wudaoliang group sedimentary rock facies and its combination, regarding lacustrine facies as principle ; the northern qiangtang suonahu formation sedimentary facies was divided for fluvial facies and the lacustrine facies, regarding lacustrine facies as principle

    根據五道梁群沉積巖相特徵及其組合，將五道梁沉積相劃分為扇三角洲- -湖泊相，以湖泊相為主。羌北盆地嗩吶湖組沉積相劃分為河流相和湖泊相，以湖泊相為主。
  11. The sedimentary facies of the jurassic penglaizhen formation in the studied area can be described as follows : from the edge of the basin, the source of deposition, to the center of the sedimentation are alluvial fan facies fluvial facies fan delta facies delta facies lake facies and lake floor fan facies in turn

    研究區侏羅世蓬萊鎮期沉積盆地的沉積相類型分佈，從盆緣近物源區至盆地沉降-沉積中心區依次為沖積扇、河流相、扇三角洲相、河控三角洲相、湖泊相和湖底扇相等沉積體系。
  12. The latter is further sub - divided into gravelly and sandy braided fluvial facies

    其中辮狀河可劃分為礫質辮狀河和砂質辮狀河。
  13. Study on three dimensional spatial distribution model for interlayer in fluvial facies reservoir

    河流相儲集層夾層的三維空間分佈研究
  14. In the early term ( sa, sb ) and the late term ( se ) of abu garbra, the fluvial facies and delta facies were deposited

    河流相和三角洲相主要發育在abugvarbra組sa 、 sb和se層序發育期。
  15. The types of sedimentary facies were mainly fan - shaped delta, delta, binshore subaqueous fans, slump turbid fan, lake facies, fluvial facies

    該研究區主要發育扇三角洲、三角洲、近岸水下扇、滑塌濁積扇、湖相和河流相沉積。
  16. According to the idea of analytical hierarchy process, using structure element analytical method combining outcrop studies, for anatomizing in - layer short lap, to study in detail shengli oil field fluvial facies sand body internal building structure, the complete set reservoir bed can be divided in to single sand bed at highly asymmetrical longitudinal direction and described to microfacies and single sand body at flat

    摘要以層次分析思想為指導，應用結構要素分析法，結合露頭研究，解剖層內薄夾層並對砂體內部建築結構進行詳細研究，認為這樣就可以預測性地描繪出勝利油區河流相單砂體的幾何形態、連通性、以及儲層非均質性，準確判斷出砂體的成因類型，揭示了砂體內部建築結構特徵。
  17. Starting from sedimentary characteristics and connecting relation of sandbody, and by applying fluvial facies sedimentary theory, the geological characteristics of different kind of response wells in polymer flooding test area at south part of lamadian oil field is analyzed, as a result the reasons affecting polymer flooding effect is made clear, all these provide basis for making polymer flooding plan and behavior analysis

    應用河流相沉積理論，從砂體的沉積特徵和連通關系入手，分析了喇嘛甸油田南塊注聚合物試驗區不同類型見效井的地質特徵，從而搞清了影響聚合物驅效果的原因，為今後編制聚合物驅方案及動態分析提供了依據。
  18. In this paper, oil reservoir fine description has been applied, and by study of reservoir, structure and fluid features, fluid units have been divided and new geology models have been rebuilt. then logging data have been reinterpreted and reprocessed and numerical modeling results have been used. on base of these work, the residual oil distribution feature and regulation in the fluvial facies sandstone in gudao oil field south region has been scientifically studied

    本文主要運用油藏精細描述技術，通過儲層、構造、流體研究，劃分出流體流動單元，重建新的地質模型，在此基礎上對測井資料進行了重新解釋和處理，並運用數值模擬研究結果，對孤島油田南區河流相砂巖油藏剩餘油分佈特徵和分佈規律進行了科學研究。
  19. The reservoir is sand of silurian and jurassic especially of delta and distributary fluvial facies sand. the growth of well reservoir sand is the key fector for gas reservoir to form in this area. by the small porosity of silurian compact sand, the position where comparative homogeneous sand growth with little mud or fracture concentrated is the location for gas to enrich

    該區儲層為中上奧陶統、志留系、侏羅系和白堊系砂巖，但以侏羅系的三角洲和扇三角洲相水下分流河道砂體、濱湖相灘壩砂體和志留系濱岸砂巖為主要目的層。
  20. Pi formation is combination of thick sand body, because the sediment mode of reservoir in changyuan of daqing is mainly combined of great leaf delta and partly fluvial facies, about 500m thick, combined of 130 little sand or mud layers, which is typical heterogeneity reservoir, the reservoir ' s character is greatly distribute, high permeate and serious heterogeneity

    Pi油層組是厚油層組合，由於大慶長垣儲層的沉積模式以大型葉狀三角洲及部分河流相為主，總厚度500多米，由130多個小砂層和泥巖交互而成，是一套典型的非均質砂巖儲層，該儲層具有分佈廣、厚度大、滲透率高和層內非均質性嚴重等特點。
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