潮上坪 的英文怎麼說

中文拼音 [cháoshàngpíng]
潮上坪 英文
supratidal flat
  • 潮 : Ⅰ名詞1 （潮汐; 潮水） tide 2 （比喻大規模的社會變動或運動發展的起伏形勢） （social） upsurge; cur...
  • 上 : 上名詞[語言學] （指上聲） falling-rising tone
  • 坪 : 名詞（平地） level ground
  1. Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit

    本文根據沉積學、石油地質學和層序地層學理論，綜合利用地表露頭、鉆井巖芯、測井曲線資料和試氣成果資料，對鄂爾多斯盆地塔巴廟區塊晚古生代沉積體系及含氣層特徵進行了研究。結果表明，研究區內目的層段可以劃分為2個沉積體系： （ 1 ）上石炭統太原期為有障壁海岸沉積體系，發育潮坪?瀉湖?障壁砂壩沉積。
  2. At the same time, relationship between rock and elctronics for every formation is determined. 2. there are five depositional faces in the area : open sea, restrained sea, tidal flat, salified lagoon and bank

    4 、在單井沉積相研究的基礎上，對各組的巖相古地理特徵進行了詳細研究，研究認為：區內發育開闊海、局限海、潮坪、咸化瀉湖和灘五種沉積相類型。
  3. The factors affecting bird distribution and diversity were beach width, hydrodynamic conditions and the size of effective upshore intertidal area

    影響這一區域鳥類分佈和多樣性的因素包括不同區域的灘塗寬度、水動力條件以及有效潮上坪面積等。
  4. The upper part is a set of evaporite quasi - tidal sequence with clear cycles which is made up of middle - thin - bedded, gypsum - bearing muddy limestone and dolomicrite

    上部為中薄層狀富泥的含石膏質夾層的泥質泥晶灰巖、微晶白雲巖組成的旋迴性清楚的似蒸發潮坪層序。
  5. 2. the new idea about classification of oil and gas accumulation unit for exploration have been put forward, which holds the sound basis for the perpendicular and plane position and prediction of carbonate reservoir in feixianguan guan group. 3. the depositional systems of feixianguanguan group in taphrogenic consist of carbonate platform facies ( include oolitic bar, oolitic beach, lagoon, flats ), margin shelf and trough. there are five development staged in taphrogenic trough

    3 、指出裂陷槽中飛仙關組沉積體系在平面上由碳酸鹽巖臺地相（包括灘壩相、鮞灘相、瀉湖相、潮坪相） 、陸棚相、裂陷槽相組成，裂陷槽經歷了發生期、發展期、穩定期、過渡期及衰亡期五大發展演化階段，每一階段各發育不同的沉積相，且以一種沉積相為主。
  6. ( 2 ) based on the two important sections of yanshiping and yicangma, a study is conducted on the sedimentary features and facies of middle - upper jurassic series, it is suggested that quemo formation is river - delta facies deposit, buqu formation is chiefly carbonate ramp facies deposit, xiali formation is delta - tidal flat facies deposit, ? suowa formation is mixed shelf - lagoonal facies deposits and xueshan formation is river - delta facies deposit

    （ 2 ）以雁石坪和依倉瑪兩條重點剖面為基礎，開展了中?上侏羅統沉積特徵、沉積相等方面研究，認為研究區雀莫錯組為河流?三角洲相沉積，布曲組以碳酸鹽緩坡相沉積為主，夏里組為三角洲?潮坪相沉積，索瓦組為混積陸棚?瀉湖相沉積，雪山組為河流?三角洲相沉積。
  7. The petrology revelas that the sedimentary environment of the study area is carbonate tide - flat and shallow sea which is also strongly affected by the volcanic materials and wind - brought clastics during the period of yangzhuang

    上述巖石特徵表明，研究區在中元古代薊縣紀早期的楊莊期為淺海潮坪碳酸鹽沈積環境，沈積作用受中遠源火山物質和風攜碎屑的強烈影響。
  8. The study area lies in the tidal flat of a delta - lobe which came into being between 1964 and 1976

    研究區位於1964 - 1976年黃河由刁口入海時形成的三角洲潮坪上。
  9. The lithofacies can be grouped into three types : structure upward deeping of tidal flat - shoreface dominated by tidal ; structure upward deeping of tidal flat - shoreface dominated by sandstone ; structure upward shallowing and then deeping of tidal flat - shoreface

    瑪托組垂向巖性序列可以分為三種類型，即以泥巖為主的向上變深的潮坪?濱面結構、向上變深的濱面結構和向上變淺后變深的潮坪?濱面結構。
  10. The study areas have same engineering geological environment ; one oil - field road was built for exploring petroleum to be formed a wave barrier in 1995. the hydrodynamic condition between the both of side is different

    所選定的研究區，在1995年以前工程地質條件基本上是均勻一致的；一條為石油開采而於1995年在中潮坪修築的道路導致道路兩側的水動力條件發生了明顯的變化。
  11. Six lithofacies palaeogeographic maps of doushantuo, dengying, qiongzhusi, canglangpu, and longwangmiao ages of late sinian and early cambrian have been made in the light of dominant facies and in the way to make stratigraphic map

    中揚子地區上震旦統發育了從碳酸鹽潮坪、開闊臺地、淺灘、臺地邊緣、斜坡到臺地前緣盆地等沉積，下寒武統下部主要?細碎屑巖和碳酸鹽巖組成的混合型淺海陸棚沉積，上部變成碳酸鹽潮坪、開闊臺地、臺緣斜坡和臺緣盆地沉積。
  12. Moreover, the system tracts in sequence are characterized by dualistic structure, namely transgressive - highstand system tracts, and tst > hst. the parasequences are divided into three types, which is respectively dominated by sandstones, mudstones, and shallowing - upward tidal flat system. and prograding sequence and retrograding sequence are composed of stacking parasequence set

    層序中體系域具有二元結構特徵，即海侵?高水位體系域，且tst hst ，準層序類型有三種，分別是以砂巖為主的準層序、以泥巖為主的準層序和以潮坪體系向上變淺的準層序。
  13. Phosphate deposits are distributed along the margin, platform and basin in the west yangtze area. the analysis methods include the paleogeography, petrology, organic geochemistry, geochemistry. the conclusions are drawn that the source of phosphate deposits distributed along the margin originate from the weathering production of continent, while phosphate deposits along the platform and basin gain phosphorus through hot spring on the buttom of the sea floor, which is brought to the sedimentary environment by rising sea - fluid, then accumulated by the organism and microorganism, meanwhile, basin phosphorite keep relatively higher organic carbon content

    認為早寒武世早期古陸遭受風化，被剝蝕下來的產物成為潮坪型磷塊巖的主要磷質來源，在碳酸鹽巖臺地發生的熱點活動和上升洋流從盆底深部帶來的磷質，共同作為臺地型磷塊巖的磷源，盆地型磷塊巖的磷質同樣是由熱點活動和上升流攜帶至缺氧的沉積環境中，通過藻類或微生物的富集作用成巖，並保留了較高的有機碳含量。
分享友人
分享到 Line

分享到臉書