海底特徵 的英文怎麼說

中文拼音 [hǎidezhǐ]
海底特徵 英文
character of the bottom
  • : 底助詞(用在定語后, 表示定語和中心詞之間是領屬關系, 現在多寫作「的」)
  • : Ⅰ形容詞(特殊; 超出一般) particular; special; exceptional; unusual Ⅱ副詞1 (特別) especially; v...
  • : 名詞[音樂] (古代五音之一 相當于簡譜的「5」) a note of the ancient chinese five tone scale corre...
  • 特徵 : characteristic; feature; properties; aspect; trait
  1. This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible

    按照不同構造層,研究了各構造層的構造:基構造層:受早西期構造作用的影響,與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關,為一構造變形和巖漿侵入活動強烈的古生代褶皺基。二疊系構造層:受中西區域性伸展斷陷作用的影響,盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合,如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。
  2. Due to nonlinear bottom boundary condition, the generation of internal tides over finite topography can only be deal with by using of ray - tracing method beforetime. the transforms introduced in this dissertation make it possible use eigenvalue method to investigate the generation of internal tides over finite topographies

    由於非線性邊界條件的使用,前人處理有限地形上內潮的產生問題只能求助於射線理論,本文提出的坐標變換將若干地形變換成平,從而使得利用值方法研究這些地形上的內潮生成問題成為可能。
  3. A sets of transforms are introduced in this dissertation, by using of which some kinds of topographies, such as continental slope and ridge, can be converted into flat bottom. the processing simplifies the generation of internal tides and reflection of internal waves over those kinds of topographies

    針對洋中的一些地形,如陸架陸坡地形、山地形、溝地形,提出了一組坐標變換,該變換可以將這些地形變換成平,從而使得在這些地形上內波的傳播和內潮的產生問題得到很大的簡化。
  4. Frame - building organisms mostly are sphinctozoa, inozoa, hydrozoa, tabulozoa. binding organisms mainly are bluegreen algae, tubiphytes and tabulozoa. accessory organisms are bryozoa, brachiopoda, foraminifera, echinodermata, etc. what ' s more, biota are different with various reef facies

    在各相帶內,生物組合也迥然不同,礁相以棲生物為主,盆地相以綿骨針、鈣球、放射蟲為,而礁后相則以裸松藻、有孔蟲、蜓類、棘皮類為
  5. 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

    本文根據南黃中部泥質區和東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陸架晚第四紀古環境演化、棲動物群、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、平面平均上升率,討論目前中國東部平面上升的狀況、溫室效應及岸帶保護。
  6. Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous, is featured by simple sedimentary feature, depositional cycle, small lacustrine transgressive, dry climate, salinization lacustrine water and multi - and - near sources

    摘要二連盆地是在西期地槽褶皺基上發育起來的早白堊世斷陷湖泊群,具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸化、沉積旋迴單一,多物源、近物源和粗碎屑等沉積,以及發育巖性地層油氣藏為主的油氣分佈點。
  7. Through synthetically study, some achievements are made as follows : 1. based on the application of sequence stratigraphy, for the first time the characteristics of sequence stratigraphy in the xicheng concentrated mineralization area are discussed systematically and 13 three graded imperfect sequences of devonian stratum are recognized. the result shows that hydrothermal sedimentary mineralized type and hydrothermal sedimentary - rebuilded mineralized type ore deposits occur in intergrade between two sequence, as well as occur in intergrade between highstand systems tract and transgressive systems tract

    通過對該區礦床成礦作用的綜合分析研究,取得了如下一些成果和認識: 1 )應用層序地層學理論,首次系統論述了該區泥盆系層序地層的,識別出13個不完整的三級層序,並進行了區域對比。層序地層分析發現熱水沉積型礦床和熱水沉積-改造型礦床的賦礦部位是兩個層序的過渡部位,既高水位體系域向侵體系域過渡。
  8. We find that the petrology characteristic of all the samples have no characteristic of meteoric water such as geopetal structure, infiltrative sand, ( uniform cement and gravitational cement on base of the research of the dolomite in the regions. on the dot diagram of combination of mgco3 ( mol % ) and sr, the dot are all close to the line of seawater whether they are microlite - crystalline penecontemporaneous dolostone or diagenetic dolostone of various crystals. the 87sr / 86sr value of dolostone or matrix is less than the one of sparry calcite in cave or vein, and close to the value of seawater

    通過本區白雲巖的研究發現:已有的白雲巖樣品的巖石學沒有顯示出如示構造、滲濾沙、新月型膠結物和重力膠結物等大氣淡水作用的;在白雲石mgco _ 3mol百分數和白雲石sr含量的投點圖中,無論是準同生成因的泥?微晶白雲巖,還是粉?細晶(或中晶,或細晶以上的不等晶)的成巖白雲巖,均投在水線的附近;白雲巖(或基質)的~ ( 87 ) sr / ~ ( 86 ) sr比值顯著低於與孔洞或脈中充填的亮晶方解石,且與水值十分接近, ~ ( 13 ) c和~ ( 18 ) o值顯著高於孔洞或脈中充填的亮晶方解石,也偏向于水值; mn含量則顯著低於孔洞或脈中充填的亮晶方解石。
  9. According to their space position, the seismic features of shallow gas in this region can be divided into three groups : ( 1 ) features in the stratum : acoustic blanket, acoustic curtains, acoustic turbidity, irregular strong top reflection boundary, and phase pull - down in both flanks ; ( 2 ) features of the seabed : seabed pockmark and giant sunken pit ; ( 3 ) features in the seawater column : acoustic plumes, cloudy turbidity and point - line - type reflection

    該區的淺層氣地震按空間位置分為3大類: ( 1 )地層中的:聲學空白、聲學幕、聲學擾動、不規則強反射頂界面、兩側相位下拉; ( 2 )面的麻坑、大型塌陷坑; ( 3 )水層中的:聲學羽流、雲狀擾動、點劃線反射。
  10. Based on the distributions, patterns and movement characteristics of sea bottom sand waves in china sea shelf area, the effects of sand waves on submarine cable burial operation are analyzed

    摘要基於中國大陸架區沙波的分佈、形態和移動,分析了沙波對纜施工的埋設張力和埋設深度的影響。
  11. Biogeochemical characteristics of organic carbon in surface sediments from the chukchi sea

    北極楚科奇表層沉積物有機碳的生物地球化學
  12. The landscape under oceans differs from that on the earth. it features with fluctuant landforms

    地貌與大陸地形不同,它一起伏不平的地形為
  13. According to the hydrocarbon analyses of crude oil samples an offshore oil field in china and the sea bed sediments just over this field, it is proved that the advanced technology can be used in such aspects of offshore geochemical prospecting as the correlations between oil and oil and between oil and sea bed sediments, the identification of hydrocarbon characteristics, and the estimation of traps

    摘要對中國某域油氣田原油及其上方沉積物樣品的指紋烴組分進行分析后認為,在洋油氣化探領域中的油與油、油與沉積物對比研究和圈閉油氣性質識別及圈閉評價等方面,指紋烴技術具有廣闊的應用前景。
  14. The discuss on the topographical environment characteristics of typical modern marine hydrothermal activity regions will be helpful to increase understanding of the modern hydrothermal activity, the distribution rules of its mineral resources and the forming causes and mechanism, etc

    摘要對現代熱液活動區地形環境的分析有助於增進對現代熱液活動及其礦產資源分佈規律、熱液活動成因機制等的了解。
  15. Through the systematic analysis and contrast studies on topographical environment characteristics of these typical regions, it is found that the hydrothermal activity only occurs under the circumstance of the particular topographical environment, though it distributes widely in the tensional tectonic environment, for instance, the mid - ocean ridges, transform faults zones, back - arc spreading basins and the modern marine craters regions

    通過對典型熱液區地形環境的系統分析和對比研究發現盡管現代熱液活動廣泛分佈在大洋中脊、轉換斷層、弧后擴張盆地等各種不同的張性構造環境及現代火山活動區,但也僅出現在殊的地形環境條件下。
  16. Distribution and source of heavy metal elements in sediments of zhanjiang harbor

    粵西湛江港沉積物重金屬的分佈與來源
  17. Abstract : according to the composition, the thermal - water sedimentary rocks of yinmin formation in the dongchuang copper ore field can be divided into nine types, of which skarnoid, cupric magnetite carbonate, paracontemporaneous breccia formed in thermal water processing are confirmed and named in this study

    文摘:東川銅礦田因民組熱水沉積巖根據主要成分可分為9大類,其中類夕卡巖、含銅磁鐵碳酸鹽巖、熱水膠結準同生角礫巖為本次研究確定和命名,其礦物組合、微量元素、稀土元素等地球化學表明:它們是火山噴流沉積作用的產物。
  18. For solving the problems that downward continuation of the space gravity anomaly can not be used in downward continuation of sea surface gravity anomaly, on the basis of prey principle used to compute gravity in the surface - layer of the earth, and with considering the density of sea water and sea bottom topography, two new methods are proposed

    摘要針對空間重力異常向下延拓方法不適用於面重力異常向下延拓的問題,根據珀雷原理求地球表層內部重力的方法、水密度及地形的,提出了兩種面重力異常向下延拓的演算法。
  19. Surrounding these special problems met in gas hydrates exploration and through study of high - precision magnetic survey, the sea test by r / v haiyang 1y that is owned by guangzhou marine geological survey in dongsha area of the south china sea, systematical analysis of the test result and combination interpretation of magnetic survey with seismic profile, the authors successfully employ the method to recognize the truth or false of the diapir in seismic profile by integrating total field of high - precision marine magnetic measurement with its gradient change

    本文就目前天然氣水合物調查中存在的這些殊技術問題,通過對上高精度磁力測量技術方法研究、廣州洋地質調查局「洋四號」船在南北部東沙域的上試驗、對試驗結果的系統研究分析以及磁測和地震剖面兩種手段的綜合解釋,成功地嘗試了用高精度洋磁測成果中的磁力總場和梯度變化來識別水合物勘探中高解析度地震剖面上的泥辟構造真偽的技術方法。
  20. Concentrations of total suspended matter ( ctsm ) is unanimous with observational data and other scholars " researching results. the distribution of ctsm is higher along coast than other areas there is a tongue - like zone with high ctsm from north to southeast. the transport simulation result reveals that sm can spread to the okinawa trough for enough sea water mixing in winter. but in summer. sm can not traverse the big water barrier of kushino for different circulation character. this difference is probably related to the shifting n - s monsoon

    懸浮體輸送表明,在冬季,懸浮體除了在陸架上發生擴散外,由於水的強烈混合作用和環流的季節性變化,部分中、層懸浮體可擴散至沖繩槽甚至西太平洋;在夏季,由於水層化及夏季環流,懸浮體基本不能穿越黑潮這一水障,這一差異可能是由於季風和不同環流所引起的。
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