凹陷湖 的英文怎麼說

中文拼音 [āoxiànhú]
凹陷湖 英文
downwarped lake
  • 凹 : 凹名詞（凹陷的地方, 用於地名） low-lying area; depression （used in place names）
  • 陷 : Ⅰ名詞1 （陷阱） pitfall; trap2 （缺點） defect; deficiency Ⅱ動詞1 （掉進） get stuck or bogged do...
  • 湖 : 名詞1 （被陸地圍著的大片積水） lake 2 （指湖州） short for huzhou3 （指湖南、湖北） a name referr...
  • 凹陷 : hollow; sunken; depressed; pit; inflection; swaying; deboss; sag; dished; thumbmark （禽類單冠邊...
  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. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現，紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型，並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖，以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律，比如在北部的凹陷陡坡背景下，上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系，下降半旋迴高水位期，扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下，上升半旋迴主要發育辮狀河流相，下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。
  3. Un - compensating lacustrine deposition, which is multi - resources, is dominated in the depression

    凹陷以非補償的湖相沉積為主，具有多源性。
  4. From studies of these characteristics of structures, palaeontology, drilling, well logging, seismic profile, salt chemistry and lacustrine sedimentary system, it is recognized that the new characteristics occur in of section pukou and in huaiyiri sag, and the huge thickness of salt rocks is formed by the crust salt materials upwelling along deep fracture in the form of hot bittern and entering lacustrine basin in this area

    通過該區構造、古生物、鉆井、測井、地震、鹽巖化學及湖盆內沉積體系等特徵的研究，認為淮陰凹陷浦口組二段和三段的沉積構造有其特殊性，巨厚的鹽巖層是殼深部鹽類物質沿深大斷裂上涌以熱鹵水形式進入湖盆的結果。
  5. 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。
  6. Ostracoda, and so on. in the deep lake facies of niujuanhu and mazhong structural belts, there were also discovered gravity - flow microfacies, which was mainly composed of turbidite in which the slump structure and convolute bedding were often found

    馬朗凹陷牛圈湖構造帶、馬中構造帶的半深湖相中，發育湖泊重力流微相，典型的表現為濁積巖的發育，其中可見到重力滑塌構造及包卷層理等。
  7. 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。
  8. In the condensed sections analysis, the concept of water - bearing lacustrine basin condensed sections and non - water - bearing basin condensed sections are firstly put forward, and have been described their features of lithology, mineral and geophysics, and have been predicted their distribution. meantime, this paper has studied the geochemical characters of source rocks, and contrast betwee

    同時，對有水湖泊密集段進行了烴源巖地球化學特徵和烴源對比研究，確立了凹陷的含油氣系統；對無水盆地密集段進行了蓋層封閉能力的研究，確定了含油氣系統的區域性蓋層及頂部范圍。
  9. By the influence of regional structural movement, the structure styles of mahu depression are simple, but the generation and migration of oil and gas are complex

    受區域構造運動影響，瑪湖凹陷構造格局簡單，但其對油氣形成、聚集的影響仍然比較復雜。
  10. Lacustrine dolomite reservoir in the hinterland of biyang sag is mainly distributed at no. 2 and no. 3 sections of hetaoyuan with its development controlled mainly by the lithology diagenesis and nose ? like structure

    泌陽凹陷腹部湖相白雲巖油層主要分佈在核二3和核三2段，其發育程度主要受巖性、成巖作用和鼻狀構造控制。
  11. Abstract : lacustrine dolomite reservoir in the hinterland of biyang sag is mainly distributed at no. 2 and no. 3 sections of hetaoyuan & nbsp ; with its development controlled mainly by the lithology diagenesis and nose ? like structure

    文摘:泌陽凹陷腹部湖相白雲巖油層主要分佈在核二3和核三2段，其發育程度主要受巖性、成巖作用和鼻狀構造控制。
  12. During late mesozoic and cenozoic, extensions were widespread in eastern china and adjacent areas. the induced compressions and extensions, uplifting and subsidence as well as large - scale magamatism, increased the pre - existing ne - nne trending faults, uplifts and subsidence belts. this is how ; the giant transform structure led to the formation of xihu depression

    在晚中生代與新生代，拉張作用廣泛分佈於中國東部及鄰區，導致了擠壓與拉張、隆起與沉降以及大規模的巖漿作用，於是使早先存在的北東北北東向斷層、隆起帶與沉降帶增強，這也是大的轉換斷層形成西湖凹陷地層的機理。
  13. To sum up the above analysis, we make sure that the pretertiary of haijiao uplift, yushan uplift and east flank in oujiang depression and the transitional zone between changjiang depression and xihu depression is a new prospect of time and space for hydrocarbon exploration in the shelf basin of the east china sea

    因此，海礁凸起、漁山凸起、甌江凹陷東側、長江凹陷與西湖凹陷之間以及浙閩隆褶帶的前第三系是東海陸架區油氣勘探的新領域。
  14. Shifting of lake shoreline and lithofacies palaeogeographic characters during sedimentary period of the member 3 of shahejie formation of paleogene in dongpu sag

    東濮凹陷古近系沙河街組沙三段沉積期湖岸線的變化及巖相古地理特徵
  15. High frequency lake - level change of 3rd member of shahejie formation and prediction of lowstand sand body in dongpu depression

    東濮凹陷沙三段高頻湖平面變化及低位砂體預測
  16. This paper focuses on recognizing the stratigraphic cycles caused by multi - order base - level cycles, establishing the stratigraphic correlation framework and predicting the lithological traps of the third section of shahejie formation, linnan sub - depression

    臨南窪陷位於惠民凹陷西南部，是發育在華北地臺之上的中、新生代裂谷盆地，為湖相沉積。
  17. At the beginning of tiaohu period, the lake basin shrank, and the water became shallow. braided river facies and braided delta facies were found on both side of the basin, and deep lake facies disappeared, and shallow lake facies was only found in the southern of tiaohu seg and central part of malang seg

    從中二疊世條湖期開始，湖盆發生萎縮，水體變淺，盆地南北兩側出現辮狀河及辮狀河三角洲相沉積，半深湖相消失，僅在條湖凹陷南緣及馬朗凹陷中部殘余濱淺湖相沉積。
  18. The upper tertiary oil - type gas is mainly positioned in the east of the mangai depression, the aljin slope and the southwestern faulted depression, while the upper coal - type gas in the yiliping depression, the sanhu depression and the erboliang - yikeyawuru structural belt

    上第三系油型氣主要分佈於茫崖凹陷東部、阿爾金斜坡和柴西南斷陷區；上第三系煤型氣主要分佈於一里坪凹陷、三湖凹陷和鄂博梁伊克雅烏汝構造帶。
  19. It is a late cretaceous to tertiary basin located on the eastern part of the continental shelf of the east china sea ; it occupies an area of 59, 000 km2

    西湖凹陷是晚白堊第三紀盆地，位於中國東海大陸架的東部，面積590000km2 ，處于緯度124030 '與127000 '之間，經度28030 '與31000 '之間。
  20. The fall of lake - mountain in it is low and sources are relatively farther, oil generation and accumulation conditions are poor

    凹陷湖嶺落差小物源相對較遠，生儲配置條件差，尋找油氣藏的條件苛刻。
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