沉積源地 的英文怎麼說

中文拼音 [chénjīyuánde]
沉積源地 英文
source of sediments
  • 沉 : Ⅰ動詞1 （沉沒; 墜落） sink 2 （沉下 多指抽象事物） keep down; lower 3 [方言] （停止） rest Ⅱ形容...
  • 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...
  • 源 : 名詞1. （水流起頭的地方） source （of a river）; fountainhead 2. （來源） source; cause 3. （姓氏） a surname
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. Three main rock types make up the geology of singapore : igneous, sedimentary and alluvium. where is the main source of granite found

    形成新加坡地質的三種主要巖石類型：火成巖、沉積巖和沖積巖。哪裡是花崗巖的主要來源地？
  2. In the research area, the incised valley was formed during the sea level downwards and was provided source by the arenaceous river from qiaotou. it is stacked by 3 incised valleys formed in 3 different sequences

    研究區內子洲鎮川堡地區發育的下切河谷形成於海平面下降時期，來源於橋頭的砂質河流沉積，為疊置的、形成於三個不同三級層序底部的下切河谷充填沉積。
  3. Sample ' s analyses and tests in laboratory, this thesis makes a detailed research on holocene deposits characteristics of mu us desert, especially on characteristics of grain size composition, which break through previous description of determining the nature and gain a series of number indexes. at the same time, this thesis has also researched arenaceous source on every part of mu us. firstly mu us desert ' s forming process is deeply influenced by the east asian monsoon, the grain size gradually becomes smaller, while the magnetic susceptibility becomes larger from northwest to southeast this phenomenon not only appears on the surface of mu us, but also obviously reflects on the same layer of different places

    根據大量野外詳細考察和室內樣品分析與測試，本文對毛烏素沙地全新世地層沉積特徵做了細致的探討，尤其對區域地層的粒度組成特徵做了進一步的研究，突破了以往的定性描述，得出了一系列量化指標；結合野外的考察工作，對其不同地區的沙質來源做了詳細分析，主要得出以下結論： 1 、毛烏素沙地形成過程深受東亞季風影響，粒度自西北向東南逐漸變細、磁化率值逐漸變大。
  4. Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock

    摘要以現有資料為基礎，通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究，認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化，沉積了巨厚的新生代地層，自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。
  5. Source and distribution of biogenic matter in sediments at station of chukchi sea area

    北極楚科奇海地區沉積物生源物質的來源和分佈
  6. Combination types of coexistent multiple energy resources in the ordos basin and an analysis of the upper paleozoic sedimentation control mechanism

    鄂爾多斯盆地多種能源共存富集的組合形式及上古生界沉積控制機制分析
  7. Geotectonically, the youjiang sedimentary basin was referred as youjiang yindosinian folded belt. triassic turbidites accumulated in the basin were derived from surrounding ancient lands including yuebei, jiangnan, and yunkai. tectonic setting of the sedimentary basin was in between an active continental margin and a continental island arc

    賦礦濁積巖系的主要物源區為盆地周圍的「越北古陸」 、 「江南古陸」和東邊地區包括欽防海西褶皺帶在內的「雲開古陸」 ，沉積構造背景介於大陸島弧和活動大陸邊緣之間的過渡構造環境。
  8. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃海中部泥質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ （ 14 ） c測年、淺地層剖面等，參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古水團、沉積速率、古水深、沉積物源、海平面平均上升率，討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。
  9. Meso - cenozoic great continental spreading basins and their orogeny of china and adjacent regions

    南沙海域沉積盆地及油氣資源分佈
  10. In its broadest application geophysics makes a major contribution to understanding the earth ' s crust and, especially through the application of modem plate tectonic theory, the genesis and petroleum potential of sedimentary basins

    地球物理的廣泛應用對于了解地殼，尤其是應用了現代板塊構造理論后，對于了解沉積盆地的成因和潛在石油資源作出了重要貢獻。
  11. In the link party of qinling - qiliang - kunlun belt, the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin. the bayan har basin thought to be the preexistence of the songpan - garze belt, is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic. the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ), then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic

    在秦祁昆侖結合部研究中，加強和突出了精細的島弧盆分析和造山作用關系的研究，探討了秦、祁、昆結合部多島弧盆特徵；通過巴顏喀拉地區沉積特徵，沉積體的空間展布和形態，面式物源供給方式，礦物成分和地球化學背景分析，其沉積盆地屬性總體上反映出一個從過渡地殼-洋殼基礎上發育起來的周緣前陸盆地的發展和演化過程。
  12. In its broadest application geophysics makes a major contribution to understanding the earth ' s crust and, especially through the application of modern plate tectonic theory, the genesis and petroleum potential of sedimentary basins

    地球物理的廣泛應用對于了解地殼，尤其是應用了現代板塊構造理論后，對于了解沉積盆地的成因和潛在石油資源作出了重要貢獻。
  13. 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。
  14. Much of the oil and gas resources reside in lake basins in the world including china

    世界上很大一部分油氣資源賦存於湖相沉積盆地中，特別是我國具有陸相湖盆成油的顯著特點。
  15. Basin system is the united area of the deposition space and the denudation area. the evolution of the basin system can mirror the process of the related erogenic movement. the disintegration of a basin system indicates the end of one time of erogenic movement

    沉積盆地系統是堆積空間與蝕源區的統一，盆地系統的演化反映出造山運動的歷程，一個盆地系統的瓦解是一次造山運動的完成，同時又形成了新的盆地系統。
  16. With regard to the causes of formation and sources of salt, people have different point of views in different basins, and different depositional models are set up, even in one same basin there are also divergent view to exist different opinions still exist on the position of the salt bearing strata in sequence stratigraphy. it will greatly influence the exploration level of resources in salt - bearing basin if the above doublts can not be made clear. in this way, it will be of great significance to make it clear about the above issues and the relationships about salt and oil & gas

    對于鹽巖的成因及鹽源在不同盆地有不同的認識，並建立了各自的沉積模式，就是同一含鹽沉積盆地或含鹽沉積凹陷人們的認識依然分歧很大，關于鹽巖在層序地層中的位置人們的認識依然不同，對這些問題的認識不清將極大的影響對人們含鹽盆地的能源勘探開發水平，因此搞清鹽巖的成因及其與油氣聚集的關系具有重要意義。
  17. The geochemical examination of the sandstones and mudstones from the xikang group has led us to conclude that the debris are derived mostly from the surficial rocks and their overlying deposits on the xikang - yunnan ancient land, and tectonic settings display the transition from the passive continental margin to active continental margin and finally to archipelago

    通過對西康群砂、泥巖地球化學組成特徵研究，認為其物源來自康滇古陸表殼巖及其上覆的蓋層沉積，大地構造屬性為被動大陸邊緣到活動大陸邊緣再到多島弧的轉化。
  18. The provenance analysis, as a kind of important method for the analysis on the sedimentary basin, is widely applied in deducing the sedimentary basin evolution

    物源區分析作為沉積盆地分析的一種重要方法，廣泛應用於推理各種沉積盆地演化。
  19. When the formation period of formation water is different to its host rock, its chemical property in oil layer may be entirely different to adjacent water layer

    沉積盆地中的外來水可以來源於淺部或地表，重力是其運移的主要動力。
  20. Abstract : on the basis of systematic synthesis, and study on the recent comprehensive geophysical - geochmical data, such as seismic, gravimetric, magnetic, electric, comprehensive logging, radiometric survey, this paper divides the second - order tectonic units of the basement of mezo - cenozoic sedimentary basins, the structure and basement lithology of sedimentary basims, and ascertains the sequential structre, occurrence depth, thickness and spatial distribution of the basin cover, and analyses the uranium source condition of the basement and provenance area, and the uranium content of cenozoic strata, as well as the mobilization and migration of uranium in cenozoic cover

    文摘:本文全面系統地整理和分析研究了巴楚地區地震、重磁、電法、綜合測井、放射性測量等最新的綜合物化探資料，劃分出了該區中新生代沉積盆地基底的次級構造單元、盆地結構構造以及盆地基底巖性；查明了盆地蓋層的層序結構、埋深、厚度及空間展布；分析了蝕源區和基底巖性的鈾源條件和新生代地層的含鈾性及鈾的活化遷移規律。
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