濁積扇 的英文怎麼說

中文拼音 [zhuójīshān]
濁積扇 英文
turbidite fan
  • 濁 : Ⅰ形容詞1 （渾濁） muddy; foul; turbid 2 （低沉粗重） deep and thick; muddy 3 （混亂） confused; c...
  • 積 : Ⅰ動詞（積累） amass; store up; accumulate Ⅱ形容詞（長時間積累下來的） long standing; long pending...
  • 扇 : 扇動詞1 （搖動扇子等使空氣流動） fan 2 （用手掌打） strike with the palm of the hand; slap 3 （鳥...
  1. On the east terrace - fault slope of the depression, the sedimentary mode of fan - shaped delta - slump turbid fan - deep lake facies are developed. on the long axial direction of fula depression, the southeastern groove was filled with a large scale delta which was the main sources, the other little delta limited by the 3 syndepositional fault was distributed down the slope edge of the northern sub - depression. this stage developed a favorable oil sources, reservoir and regional seal which formed the good matching relations of generation, reservoir and seal in the time - space zone

    Abugarbra組的sc和sd層序發育在邊界斷層和同沉積斷層活動劇烈、湖盆擴張期，凹陷中心發育半深湖-深湖相沉積，在凹陷陡坡發育近岸水下扇，斷階緩坡帶發育扇三角洲?滑塌濁積扇?深湖相組合，長軸凹槽和北部次凹的北部緩坡帶發育三角洲體系，此層位是有利生油層和巖性圈閉發育層段。
  2. Discovery and significance of sublacustrine slump turbidite fans in chang 6 oil - bearing formation of baibao region in ordos basin, china

    鄂爾多斯盆地白豹地區長6油層組湖底滑塌濁積扇沉積特徵及其研究意義
  3. Mudstone deposited in deep water envoirment of sq6 - sq8 is the better regional sealing bed. the deep lake turbidite regionally deposited in sq6 - sq8 with better feature

    層序6 8沉積的深水湖相泥巖是本區良好的區域性蓋層，局部區域出現的深水濁積扇砂巖物性較好。
  4. Vertically, a series of turbidite fans and fan deltas developed along eastern border of guxi contemporaneous fault zone and sandbodies were overlaped with each other

    垂向上，沿東部邊界孤西同生斷裂帶發育的一系列濁積扇和扇三角洲由於遷移擺動，砂體可以相互疊置連片。
  5. The paper divided turbidite fan in deep water from long source into braided channel microfacies, inter - braided channel microfacies, medium fan over - belt microfacies, and external fan subfacies, and divided slump turbidite which related with delta into medium fan subfacies and external fan subfacies, and summed up 15 kinds of marking of subfacies and microfacies classification. at the same time, it formed a series of effective technology of analyzing turbidite source at the base of studying region geological which combined with analyzing the content change of terrigenous debris, with the found of logging facies, and with the ancient terrestrial magnetism test and other technology means under the guidance of three - dimensional model of turbidite which has been founded already and the flat surface feature of microfacies

    將遠源深水濁積扇劃分為辮狀水道微相、辮狀水道間微相、中扇過渡帶微相和外扇亞相；將與三角洲有關的滑塌濁積扇劃分為中扇和外扇兩個亞相，並總結了濁積巖沉積劃分各種亞相、微相類型的十四種標志，分別為:巖石類型、層理類型、砂巖單層厚度、粒度結構特徵（粒度中值、分選性、概率曲線） 、生物化石、儲層物性（孔隙度、滲透率） 、泥巖隔層特徵（泥巖單層厚度、層數、顏色） 、鮑瑪層序組合和自然電位曲線特徵。
  6. 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。
  7. According to the cores and seismic data, the most important facies is fan - delta in this area, mainly developing in the top member and the bottom member developing turbidite - fan. major faults " moving intensively led to deep strata sinking

    根據巖芯、地震資料可知該時期在工區內最重要的沉積相為扇三角洲沉積體系，主要發育在上部，而下部根據地震相分析則發育濁積扇沉積體系。
  8. The main conclusions are as follows ; firstly, under the influence of three phases of episodic activities, three two - order sequences is composed of three depositional cycles and three regional unconformities ; secondly, under the control of structure activities such as fault - block activities and the influence of three - order climate cycles and source recharge, lower cretaceous can be divided into six three - order sequence ; thirdly, because fault activities is weak and fault slope is gently, fan deltas exist in steep slopes in early and later stages and subaqueous fans exist and turbidite fans exist in troughs in middle stage

    主要的結論為：其一，受三期幕式活動影響，斷陷形成了3個大的沉積旋迴和3個區域不整合面，構成了下白堊統3個二級層序；其二，受斷陷內翹傾和塊斷等構造活動的控制，以及三級氣候旋迴和物源供給因素的影響，下白堊統劃分出6個三級層序；其三，在單斷斷陷湖盆中，湖泊階段的早、晚期由於凹陷邊界斷層活動較弱，斷面較緩，陡坡可以發育扇三角洲，在湖泊階段的中期主要為水下扇砂礫巖體，並在窪槽區發育濁積扇。
  9. Lowstand fans and lowstand wedges formed in lowstand system tracts of sq5 and sq6 ( that is damoguaihe formation ) and deep water turbidite fans deposed in late trangrassive system tract and early highstand system tract are the major reservoir with good physical characteristics

    層序5和層序6 （相當于大磨拐河組下段）低水位體系域沉積的低水位楔和低水位扇及水進晚期、高水位早期出現的深水濁積扇具有良好的儲集物性，也是主要的儲集層。
  10. On the basis of the framework of chronostratigraphic sequence and the analysis of well - log, seismic section, the paper studied types and the distribution of sedimentary facies. three types of sediment can be identified : braided river delta systems mainly formed on the south slope. little - sized turbidit fan mainly formed in the middle deep area and dan delta mainly formed on the north slope of the depression

    在等時層序地層格架的基礎上，通過測井、地震資料分析，對凹陷沉積相的類型及空間分佈進行了研究，研究表明南坡主要發育辮狀河三角洲體系，深窪區發育小型濁積扇體系。北坡主要發育扇三角洲相。
  11. 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。
  12. The lithological traps related to jishan delta ? turbidite fan depositional system inherently developed during the base level falling period of c3 cycle and the base level rising period ; the lithological traps related to the underwater fan depositional system near xiakou fault developed during c2 cycle ; the lithological traps related to qudi fan delta developed during the base level falling period of c2 cycle ; and there are a few lithological traps related to shangfeng delta. these predicted traps are mainly distributed in the deeply low - lying areas

    在沉積體系、沉積相研究的基礎上，對臨南窪陷沙三段巖性圈閉分佈作出了預測，指出了各旋迴基準面下降期是尋找巖性圈閉的有利層序地層位置， （扇）三角洲前緣滑塌作用或快速充填作用形成的濁積扇或滑塌作用形成的濁積巖體是巖性圈閉形成的主要場所。
  13. The most favourable sequences for subtle traps are cycle 3 and cycle 4, and the most favourable oil and gas - pool forming regions are jishan sandstone, fan - delta sandstone of south part of linnan sag, sliding turbidity sandstone of the slope part of shuangfen delta front and turbidity and sub - fan near fault of jiangjia dian

    基山砂體、臨南窪陷南部沙三下扇三角洲砂體、雙豐三角洲前緣的斜坡地帶的滑塌濁積巖砂體和江家店地區的濁積扇體和近岸水下扇體是最有利的勘探目標區。
  14. The distribution of depositional facies in bonan sag is very complex, which include five depositional systems, such as salt lake of deep water, transgressive fan delta, proximal turbidite fan, slump turbidite fan, distal turbidite fan

    窪陷內的沉積相帶展布比較復雜，發育有深水鹽湖、水進型扇三角洲、近岸濁積扇、滑塌濁積扇及帶供給水道的遠岸濁積扇等5種沉積體系。
  15. According to the difference of the genetic mechanism, it is further divided into the slump turbidite fan and the deep - water turbidite fan for they have some differentces in seismic profile, depositional character and space distribution

    根據其成因機制上的差異，又可進一步分為滑塌濁積扇和深水濁積扇等兩種沉積類型，二者在地震反射特徵、沉積特徵及空間展布上均有一定的差別。
  16. The further study on the fan is very important for the future explorition. the fan delta front around the well tiel6 is worse than the bottom shahejie formation ' s fan. the reservior ' s quality in the dawan area is relatively bad

    而沙三下的上部扇三角洲與其下部的濁積扇砂體也是一套非常有利的儲層，加強該扇體的研究對今後的油氣勘探十分重要；其次為鐵16井附近扇三角洲前緣沉積；而大灣地區儲層相對較差。
  17. Observation from 3d visualization technology indicates that although shi - 1 well has not penetrated the main part of a turbidity, it did encounter the margin of the turbidity sand body. that demonstrates area around shi - 1 well is one of the potential areas, which are likely accumulating oil and gas

    從三維可視化結果看，時1井在沙三段、沙一、二段雖然沒有鉆到濁積體主體，但也鉆過了濁積扇砂體的邊緣，而且油氣顯示良好。
  18. From comprehensive analysis, the conclusion can be drawn that the favorable reservoir of the upper part of the forth member of shahejie formation of bonan sag is the outer fan sandbody of fan delta near the y159 of the eastern part of the sag, the middle fan and outer fan of y160, midian fan and distal fan of proximal turbidite and slump turbidite

    綜合分析認為，有利儲集相帶為窪陷東部深窪區附近的義159井區扇三角洲扇端砂體、義160井區扇三角洲的扇中及扇端砂體、近岸濁積扇及滑塌濁積扇的中扇及外扇砂體。
  19. There were fan - delta, turbidite - fan, shallow - lake, shore - marsh, semideep - lake and volcano - debris facies. in the area of the well ou39 and ou44, fan - deltas developed both in the middle and the top strata of the third member of the shahejie formation. the former lies in the north area of the well ou39, belonging to the steep - slope style which was controled by inertia factor

    在歐39 、歐44井區，沙三中和沙三上均發育扇三角洲沉積，前者具以慣性因素控制的陡坡型為特點，分佈范圍相對較小，位於歐39井以北的地區；而後者以摩擦因素控制的緩坡型為特色，分佈范圍廣；而沙三下在該區則發育了一套濁積扇體，這一規律正好體現了構造演化特點對沉積充填型式及相展布的控製作用。
  20. 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。
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