蒸發巖 的英文怎麼說

中文拼音 [zhēngfāyán]
蒸發巖 英文
evaporite rocks
  • 蒸 : Ⅰ動詞1. （蒸發） evaporate2. （利用水蒸氣的熱力使食物熟或熱） steam Ⅱ名詞[中醫] （將藥物隔水蒸熟） steaming
  • 發 : 名詞（頭發） hair
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 蒸發 : [物理學] [化學] evaporation; evaporate蒸發計 evaporometer; evaporimeter; atmidometer; atmometer; ...
  1. Besides lava flows, etna produces an almost constant, rhythmic discharge of steam, ash and molten rock

    除了熔巖流，埃特納也幾乎穩定、有節奏地噴發蒸汽、火山灰和熔融的巖石。
  2. The dark green tints in the south of wales and the gloucestershire area reflect high strontium values associated with evaporites.

    位於南威爾士和格洛斯特郡地區的暗綠色反映了與蒸發巖有關的高鍶值。
  3. In middle and late periods of the early permian, the pre - caspian areas rose successively, the climate became dry, and the environment turned to be supratidal zone ( evaporitic environment ), resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite

    早二疊世中後期由於持續構造抬升，盆地氣候變得乾旱，海水變淺，潮上帶蒸發環境發育，以致這一時期廣泛發育鹽類沉積，形成含鹽層系，主要由鹽巖和硬石膏層構成，並形成許多大小不等的鹽丘構造。
  4. The middle part is a set of large tidal range tidal sequence including oolitic shoal fades which is made up of bedded - oolite dolomite and oolite limestone, gypsum - tidal fades in sabkha environment which consists of bedded gypsolyte, and gypsolyte - bearing gypsum - dolomite tidal facies

    中部為層狀鮞粒白雲巖、鮞粒灰巖的潮下鮞粒灘相與薩布哈環境的富層狀石膏巖的膏坪相、含石膏巖的膏雲坪相組成的大潮差蒸發潮坪層序。
  5. This thesis emphasizes to proceed the study on the mechanism of formation of the reservoirs of lower palaeozoic burial hills in the regions of zhuangxi and chengdao from the angle of geochemistry. the research of petrology reveal rock types of the regions mainly include carbonate rock, claystone, siltstone, breccia and a few of evaporite rock

    巖石學研究表明，樁西、埕島地區下古生界古潛山儲層的巖石類型有碳酸鹽巖、粘土巖、碎屑巖、以及少量蒸發巖，其中碳酸鹽巖是該區下古生界古潛山儲層最主要的巖石類型，為一種穩定地臺型海相沉積環境的產物。
  6. The lower part is a micro - tidal range evaporative tidal sequence consisting of thin - bedded gypsum - bearing, muddy - limestone and dolomicrite

    下部為薄層的含石膏、硬石膏晶體、團塊及腸狀石膏層的泥晶灰巖、微晶白雲巖組成的小潮差蒸發潮坪層序。
  7. 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。
  8. Another hypothesis to the existence of monomineralic evaporites is to assume the existence of separate basins of evaporation.

    另一種解釋出現單礦物蒸發巖的假說是假定存在分隔的蒸發盆地。
  9. The widespread progradationally deposited cycles are often capped by oolitic shoals, tidal flat or sabkha evaporite strata.

    廣布的加積沉積旋迴、經常被鮞灘，潮坪或薩勃哈蒸發巖層所覆蓋。
  10. Characteristics of evaporite generated in deep water of sha4 member in dongying sag

    東營凹陷沙四段深水成因蒸發巖特徵及其與油氣藏的關系
  11. Based on the distribution of the unknown compounds " x " ( between ts and tm ) in oils and rocks, in combination with the theory of gas - washing evaporative fractionation, the formation of the light oils in kela 2 - 3 dry gas reservoir is explained

    根據萜烷中未知「 x 」化合物在原油中分佈的普遍性和在烴源巖中的分佈特徵，結合氣洗蒸發分餾作用的原理，解釋了克拉2 - 3號干氣藏中少量輕質油的成因。
  12. In winter, moisture evaporating from the chalk leaves behind patches of powdery white salt crystals on the surface

    至冬日，水分蒸發，青灰巖惡地形到處都是鹽巴的白色粉末結晶，也是一獨特景觀。
  13. The light oils originated from high mature rocks. in the process from source to trap with gas washing and evaporative fractionation, the oils got rich in aromatic compounds and poor in other compounds, which indicates that gas washing has great effects on the oil compositions

    認為這些輕質油來自高成熟的烴源巖，在其運移過程中受到氣洗，發生蒸發分餾作用，使得其輕組分中芳烴化合物苯和甲苯相對富集，而其它組分則大量損失，表明了氣洗對油的改造是十分強烈的。
  14. It is considered that the sequence evolution in the palaeozoic went through the following three stages, the filling of evaporate platform, the filling of carbonate and detrital rock mixed deposits in epiric sea, and the filling of detrital deposits of lake - deltas in paralic inland sag

    認為研宄區古生界層序演化經歷了以下三個階段：蒸發臺地充填階段、陸表海碳酸鹽巖與碎屑巖混合沉積階段，以及近岸內陸坳陷的湖泊三角洲碎屑巖沉積階段。
  15. As each human begins to embody all elements including air, water, fire and earth along with the inverse elements of ether, vapor, smoke and lava, humanity will begin to thaw out as there will be enough fire to allow for an internal shift within each.

    當每個人融合入所有的元素包括氣，水，火和土，連同逆元素如以太，蒸汽，煙和熔巖時，人類將開始解凍，因為這將使每個人的內部被充分點燃（擁有足夠的能量）而允許一個內在轉換的發生。
  16. Ecological characteristics of pogonatherum paniceum ( lam. ) hack. indicated that the transpiration was reduced by its small leaf area, and inner rock water can also be up taken because of its strong roots system. therefore, it could grow on rock surface and rock aperture

    金發草生態特徵分析表明，其葉片面積較小，減少了葉的蒸騰，降低水分的散失；根系發達、根厚而平展，可在巖石表面或巖石縫隙生長，根系可吸收巖石表層和縫隙中的水分，對乾旱具有較強適應能力。
  17. Sedimentary environment in benxi stage from east to west were respectively shallow - sea muddied continental shelf, barrier island, lagoon and tidal flat. most area in taiyuan stage was distributed by shallow - sea continental shelf, but the northern and southeastern part were scattered by clastic tidal flat and carbonate tidal flat. sedimentary environment in shanxi stage, in the middle and late shihezi stage was deltas and lake

    馬5晚期研究區發育蒸發臺地相和局限臺地相；本溪期自東而西發育淺海泥質陸棚、障壁島、瀉湖及潮坪相；太原期大部分地區發育淺海陸棚沉積，北部和西南部則發育碎屑巖潮坪和碳酸鹽潮坪沉積；山西期和石盒子中晚期為三角洲和湖泊沉積環境；石盒子早期廣泛發育辮狀河三角洲和湖泊沉積。
  18. The feixianguan formation of evaporative carbonate platform is a set of sulfate - bearing evaporative tidal sediments with aboundant dolomite

    飛仙關組蒸發臺地為一套含硫酸鹽的富白雲巖的蒸發潮坪沉積層系。
  19. Main diagenesis of carbonate reservoir as following : ( 1 ). there are five types of dolomitization : evaporative pumping, seepage reflux, mixing and deep buried. ordivician main type of dolomite of qianmiqiao buried hill in dagang oilfield is elogenetic micrite and microspar dolomite

    5 、對碳酸鹽巖儲層的成巖作用分析認為： （ 1 ）白雲巖化作用有四種類型：蒸發泵白雲化作用、迴流滲透白雲化作用、混合水白雲化作用、深埋藏白雲化作用。
  20. Squyres and other team members suggest that the layered deposits they saw on these rocks could have formed from volcanic dust that either mixed with water vapour or acquired a thin coating of water at some later stage

    斯奎爾斯和其他工作人員在這些巖石上發現了分層沉積，他們推斷這可能是由火山灰與水蒸氣或晚些時候覆蓋于地表的淺水層混合而形成的。
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