正常沉積 的英文怎麼說

中文拼音 [zhēngchángchén]
正常沉積 英文
normal sedimentation
  • : 正名詞(正月) the first month of the lunar year; the first moon
  • : 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...
  • : 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...
  • 正常 : normal; regular; average
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. The pathology characteristic that liver fiber changes is collect there are many fibre hyperplasia and deposit inside abbacy and liver flocculus, but have not form the interval inside flocculus, liver cirrhosis has false flocculus to form, central vein area and collect abbacy occurrence interval, the normal structure of liver is destroyed, liver fiber changes further progress to be liver cirrhosis namely

    肝纖維化的病理特點為匯管區和肝小葉內有大量纖維組織增生和,但尚未形成小葉內間隔,肝硬化則有假小葉形成,中心靜脈區和匯管區出現間隔,肝的結構遭到破壞,肝纖維化進一步發展即為肝硬化。
  2. However, only did a few pollen germinate in inter - specific hybridization between cerasus fruticosa and c. avian and many pollen tubes are crosswise on stigma and couldn " t penetrated into style. although a few pollen tubes entered, they couldn " t continue to grow due to accumulation of callosity in pollen tubes. in view of above - mentioned results, the irregular growth of pollen was the main reason to cause the incompatibility of distant hybridization between cerasus fruticosa and c. avium

    而草原櫻桃與歐洲甜櫻桃種間雜交授粉后花粉在柱頭上雖少量萌發,但花粉管在柱頭上橫向生長,或盤繞,扭曲不能伸入花柱;個別進入花柱的花粉管先端因胼胝質而中途停止伸長未能進入子房到達胚珠,從而說明這種雜交授粉后花粉管的不行為是導致草原櫻桃與歐洲甜櫻桃遠緣雜交不親和的主要原因。
  3. The field observation of the sediments of storm surge produced by no. 11 typhoon in 1997 shows that sedimentation rate of storm surge sediments are greater than that of normal astronomical tide sediments, and the grain size shows relative coarse with poor sorting. vertical sequences of the storm sediment show parallel bedding and overlapped by hummock bedding. these characteristics provide good basis for building the index of storm surge deposit

    通過對梁垛河閘9711號臺風的現場觀測並結合目前已有的風暴潮的研究,分析了風暴潮在構造和結構上的特點,從而建立了潮灘中風暴潮的識別標志,同時在野外觀測中還發現即使在風暴潮期間,高潮灘上部仍存在只有淤沒有侵蝕的地帶。
  4. Taowan conglomerate was formed with underwater seismism at early cambrian period and consists of shattering sedimentary rock, tsunami rock, seismic turbidite and seismic volcanic rock. the shattering sedimentary rock consists of folded rock, cracked rock and autobreccia. the seismic turbidite is located in the south of luonan ductile shear zone and is called the narrow taowan conglomerate. contrarily the broad taowan conglomerate consists of shattering sedimentary rock, tsunami rock located in the north of the zone. the seismic sequence of shattering sedimentary rock - tsunami rock - seismic turbidite - seismic volcanic rock - normal sedimentary rock was first found in luonan shanxi and is rare among the reported examples about it, so it is a good example and offers power evidences to study how the southern marginal basin of huabei plate transferred to qinling orogenic belt

    震濁巖分佈於洛河韌性剪切構造帶之南,屬傳統"陶灣礫巖"范圍和涵義,即為狹義陶灣礫巖而廣義陶灣礫巖包括分佈於洛河韌性剪切構造帶之北的震巖海嘯巖及狹義陶灣礫巖。陜西洛南地區首次發現的震巖海嘯巖震濁巖震火山巖背景地震序列之完整在所報導古地震作用序列當中實屬罕見,為華北地塊南緣造山過程及深入了解古地震作用提供了良好地段和有力證據。
  5. Carbon and oxygen isotope data show that the carbonatite layer in fozichong ledge is different from the normal marine sedimentary carbonatite, infering that its formation has relation with hot - water sedimentary activity

    碳、氧同位素顯示,佛子沖礦田賦礦層位中的碳酸鹽巖地層與的海相碳酸鹽巖不同,其成因與熱水活動有關。
  6. Potential fossils are relatively rare in the final deposits of normal quartz-sand beaches.

    的石英質海灘的最終物中隱匿的化石還是比較少的。
  7. Because the volcanics and sedimentary rocks alternated with one and another, the volcanic activity of these two periods had the characteristics of many a time, multipoint of erupting

    火山巖與正常沉積巖相間分佈,且火山角礫巖發育,因此這兩個時期火山活動都具有多期次、多點噴發的特點。
  8. Abstract : yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    文摘:陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲油田,儲集層主要為三角洲砂體,壓實作用和膠結作用強烈,儲層非均質性非嚴重,因此預測次生孔隙發育帶是尋找油氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析,認為陜甘寧盆地延長統次生孔隙的形成除了受有利相帶控制外,還與地層異壓力的作用密切相關.研究認為隴東地區異壓力的形成機理主要由於成巖過程中粘土礦物脫水作用.粘土礦物大量脫水時間好與有機質脫羧期相一致,從而在異壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中,並沿著有利儲集相帶運移,在酸性水經過的地方形成大量的次生孔隙,為後期油氣運聚提供有利通道及宿住空間,從現今的勘探結果來看,通過研究地層異壓力縱橫向分佈特徵,並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  9. Yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲油田,儲集層主要為三角洲砂體,壓實作用和膠結作用強烈,儲層非均質性非嚴重,因此預測次生孔隙發育帶是尋找油氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析,認為陜甘寧盆地延長統次生孔隙的形成除了受有利相帶控制外,還與地層異壓力的作用密切相關.研究認為隴東地區異壓力的形成機理主要由於成巖過程中粘土礦物脫水作用.粘土礦物大量脫水時間好與有機質脫羧期相一致,從而在異壓力作用下將生油巖中的大量有機酸及co2帶到與之相鄰的儲集層中,並沿著有利儲集相帶運移,在酸性水經過的地方形成大量的次生孔隙,為後期油氣運聚提供有利通道及宿住空間,從現今的勘探結果來看,通過研究地層異壓力縱橫向分佈特徵,並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  10. It was also indicated by the studies on a large number of pb isotope that pb in ores of the deposit chiefly came from volcanic rocks in the strata and later intrusions with derivation of a little pb from the normal deposit stratum

    大量pb同位素研究也表明,礦床的礦石鉛源跨越了下地殼、地幔和造山帶演化線,形成混合鉛帶,多集中於地幔和造山帶演化線附近,暗示pb主要來自地層中的火山巖和後期的侵入巖,少量來自正常沉積地層。
  11. By looking into the cores, analyzing of granularity and ichno - fossils, the paper has ascertained the basin as a normal fluvial delta deposital system, which amends the former view that believed the basin should be a fan - delta system

    通過本區大量的巖心觀察、粒度分析、遺跡化石分析,修改了前人認定的其為扇三角洲體系的觀點,將其確定為的河流三角洲體系。
  12. An abnormal condition in which calcium salts are deposited in a part or tissue of the body

    鈣質著鈣鹽于體內某一部件或組織的不狀況
  13. Though the creep settlement is n ' t easy to detect, through accumulating, it will affect directly the stability of projects and even destroy the structures

    蠕變降雖然不易察覺,但經過長期累,卻能直接影響建築地基的穩定性,對工程的運行及安全構成威脅。
  14. Under the guidance of new principles and methods of modern sedimentology, detrital petrography, reservoir geology, diagenesis, this thesis has carried out detailed study on paleogene formation correlation, sedimentary environment, characteristics of sedimentary facies and diagenesis of the eastern kuche depression, tarim basin, dina area being taken as the main target of the study. based on the core, geology logging, log and seismic data from 9 typical wells, combined with the data of the adjoining area, the dominant sedimentary types of the study area have been recognized and illustrated, such as fan - delta, lacus and normal delta. in terms of the analysis on the sedimentary facies of typical and connecting wells in different areas and facies belt, together with the paleogene tectonic evolution characteristics of foreland basin, the distribution and evolution of the sedimentary facies of the study area have been clearly discovered both vertically and laterally

    通過對該區9口井的巖芯、錄井、測井、地震資料及鄰區資料的分析,識別並闡述了庫車坳陷東部下第三系的幾種主要的相類型,如扇三角洲相、湖泊相和三角洲相;通過對不同地區、不同相帶典型井及連井的相分析,結合前陸盆地在下第三系的構造演化特點,弄清了迪那地區下第三系相的縱橫相發育展布和演化規律,並建立了相模式;同時,初步開展了成巖作用、儲層孔隙演化和儲層發育模式的研究工作,科學合理地解釋了現今迪那地區下第三系儲產層主要發育在粉砂巖中的特殊現象,首次建立了下第三系儲層的發育演化模式,為庫車坳陷東部地區進一步尋找下第三系大儲量、高產油氣藏和有利的勘探區塊提供科學的、可靠的和最直接的地質依據。
  15. If there is no efficient way to control the account receivable aggradation, it will be more and more while the quantity of sales is bigger and bigger, and it will affect the normal produce

    但賒銷量過大,內部管理控制不到位容易造成應收賬款數額較多,影響企業生產經營。
  16. Fig. 1 normal culture group with the addition cerium ions : myocardial cell shows normal ultrastructure. no cerium deposits are observed in the cell

    圖1培養加鈰組:心肌細胞超微結構,細胞內無鈰顆粒。
  17. The best process for high quality tio _ ( 2 ) thin film deposited on k9 glass by reb is studied by using orthogonal test method, the se results indicate that the best process for tio _ ( 2 ) thin film deposition is the substrate temperature of 300, the total gas press in the chamber of 2 x 10 ~ 2pa and the deposition rate of 0. 2 nm - s - 1, of which the substrate temperature has influence on the optical properties of the deposited films notably

    文中首先以tio _ 2薄膜的折射率和消光系數為研究對象,採用l9交試驗法研究了在k9玻璃上制備高光學質量tio _ 2薄膜的最佳工藝條件。橢圓偏振儀的測試結果表明,制備tio _ 2薄膜的最佳工藝條件為:基片溫度300 ,工作真空2 10 ~ ( - 2 ) pa ,速率0 . 2nm ? s ~ ( - 1 ) ,其中基片溫度對薄膜光學數的影響最大,該結果具有較好的可重現性。
  18. Atypical gravity sediment

    重力
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