堊化 的英文怎麼說

中文拼音 [èhuà]
堊化 英文
chalking
  • : Ⅰ名詞(白堊; 白土) chalkⅡ動詞[書面語] (用白堊塗飾) cover with chalk; chalk
  1. For this purpos, from the point of the log geology, aimed at the actuality of the current fractured reservoir log geology interpretation and evaluation, based on synthetical analysis of the current domestic and foreign fruit of fractal dimension investigation of reservoir fracture, using the method and technique of fractal dimension, through the further discussion of the fractal dimension characteristics of m index and n index in the log interpretation archie model in a sample way and through the theoretic reasoning to the fractal dimension dfa and m index of fractured reservoir interval ' s log curve, according to the geophysical signification of the fractal dimension dfa of fractured reservoir interval ' s log curve shape : the more complicated the change of the curve shape is, the larger the its dfa value is, then the more complicated space structure of fracture and pore, then the higher value of m index of space structure of fracture and pore, and so on, the text propounds an improved method, based on box dimension, of covering log curve with scale grid, and by programming computes the dfa and its m index value of fractured reservoir interval ' s log curve, for instance, ac and rt curve, ect, then further puts this technique into application investigation, and makes analysis of application effects in the reservoirs located in l area of qx oil field from three aspects : 1. the dfa and its m index value of fractured reservoir interval ' s log curve, for instance, ac and rt curve, ect, which are derived from computing, is used to identify reservoir type by crossplotting m index with the product df _ acrt of fractal dimension of acoustical wave log curve and restivity log curve and by experiential discriminance plate of reservoir type in l area of qx oil field

    因此,對該區裂縫性儲集層的類型識別、孔滲特徵的測井地質解釋以及儲層裂縫的發育和分佈規律進行深入的研究便成為本文研究的出發點。為此,本文從測井地質的角度,針對當前裂縫性儲層測井地質解釋與評價的現狀,在綜合分析當前國內外儲層裂縫的分形分維研究成果的基礎上,利用分形分維方法和技術,通過對archie測井解釋模型中的m指數、 n指數的分形分維特性的深入淺出的論述以及裂縫性儲層段測井曲線分維d _ ( fa )與m指數的理論推導,根據裂縫性儲層測井曲線形態分維值的地球物理意義? ?曲線變越復雜,則其分維值d _ ( fa )越大、裂縫孔隙空間結構越復雜、裂縫孔隙空間結構指數m值越高等特徵,提出了改進的基於盒維數的測井曲線網格覆蓋法,編程計算了裂縫性儲層段常規測井曲線(如聲波和電阻率曲線)上分形分維值及其m指數值,進而從以下三個方面對qx油田l區塊的裂縫油藏進行應用研究,效果十分理想: 1將計算得到的可變的m指數與聲波和電阻率分維之積df _ acrt進行交繪,採用儲層分維值分類技術統計分析這些參數變的規律,並結合qx油田l區塊儲層類型經驗判別圖版,從而實現qx油田l區塊下白統的裂縫性儲層的類型識別。
  2. Therdly because of the influence of terrain and geological structure, arenaceous resources of different regions are different in mu us. sands are mainly from riverway in northwest ; from efflorescent cretaceous sandstone on account of higher topography in the middle part of mu us ; and sands resources are intricated in southeast, mainly including riverway sands, sands blown by the wind and embedded sands under so

    3 、毛烏素沙地因受地形和地質構造影響,不同區域的砂質來源情況不盡相同,西北部地區主要為河道沙;中部地區地勢較高,為白系基巖裸露而風成沙;東南部地區沙質來源情況復雜,主要有:現代河道砂、風積沙、也有埋藏在現代壤土之下的出露古沙。
  3. Distribution law of groundwater hydrochemical type in the ordos cretaceous artesian basin

    鄂爾多斯白系地下水盆地地下水水學類型的分佈規律
  4. Only in the tropics were numerous late cretaceous groups extinguished during peaks in their evolution.

    只是熱帶地區才有大批晚白紀生物類群正值其演的極盛時期突然消亡。
  5. Recently, a series of the feathered dinosaurs have been found from the jehol biota of western liaoning, northeast china, which give extremely strong evidences of the theropod hypothesis of bird origin and of the cursorial hypothesis of the avian flight origin. but the origin and early evolution of feathers have still been unanswered. in late 2000, a well - preserved specimen of dromaeosaurids was excavated from the early cretaceous jiufotang formation of shangheshou, suburb of chaoyang city, western liaoning

    2000年,遼西朝陽市上河首早白世九佛堂組地層中,發現了一件保存完好的長有羽毛的奔龍類石,這是繼北票四合屯、朝陽下三家子、凌源大王杖子之後長羽毛奔龍石在遼西的又一次發現,為解決奔龍類的系統關系、羽毛的起源及早期演提供了重要的實物資料。
  6. Climatological data from fossil pollen, leaves and wood indicate that the cretaceous forests of northern alaska consisted of a mixed canopy that included deciduous conifers with an understory of flowering plants, ferns and cycads

    由花粉、葉子和木材石?集到的氣候資料顯示,阿拉斯加北部的白紀森林有混合型林冠,包括了落葉針葉林以及林下的開花植物、蕨類和蘇鐵。
  7. 4. it is the first time that eclogite conglomerates are discovered in maotangchan and fenghuangtai formations. this suggests that ultra - high pressure metamorphic rocks in the dabie orogenic belt exhumed to the earth ' s surface in lower cretaceous. the geochemistry data indicates that the protoliths of the eclogite gravels formed in a structure setting of volcanic arc

    首次在毛坦廠組、鳳凰臺組中發現了榴輝巖礫石,這一發現表明大別造山帶超高壓變質巖在早白世已經折返到地表,而且地球學研究表明這些榴輝巖礫石的原巖形成於巖漿島弧構造背景。
  8. 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

    摘要二連盆地是在海西期地槽褶皺基底上發育起來的早白世斷陷湖泊群,具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸、沉積旋迴單一,多物源、近物源和粗碎屑等沉積特徵,以及發育巖性地層油氣藏為主的油氣分佈特點。
  9. The hanging wall of sag extended in southeast direction, with the tulage fault being the boundary fault. yinggete - bagemaode metamorphic core complex developed adjacent to northwest of chagan sag, which evolved from late jurassic to cretaceous with three - layer construction style. the kinematics mechanism of metamorphic core complex and chagan sag is a simple shear model, chagan sag extended and faulted as the metamorphic core complex rised

    在查干凹陷西北側發育英格特?巴格毛德變質核雜巖帶,可能具有三層結構模式,其形成與演時代為晚侏羅世末?白紀;該變質核雜巖與查干凹陷的運動學機制為統一的簡單剪切模式;在變質核雜巖隆升的同時,查干凹陷發生伸展斷陷。
  10. The flare of the gas - jets, the open trunks, suggestive of travel and display, the scattered contents of the make - up box - rouge, pearl powder, whiting, burnt cork, india ink, pencils for the eyelids, wigs, scissors, looking - glasses, drapery - in short, all the nameless paraphernalia of disguise, have a remarkable atmosphere of their own

    耀眼的煤氣燈,打開的箱子令人想起旅行和排場,散亂的妝用品-胭脂珍珠粉白粉軟木炭墨汁眼瞼筆假發剪刀鏡子戲裝-總之,各種叫不上名來的妝用的行頭,應有盡有,各有自己獨特的氣息。
  11. Xiongcun copper - gold ore deposit is located in gangdese metallogenetic belt with a large scale. the ore body mainly exists in the second lithoid unit ' s tuffs and the third lithoid unit ' s dacite tufa of the cretaceous volcanic stratum, which are not only mother rock but also mineralized body

    雄村銅金礦床處于岡底斯成礦帶,礦床規模巨大,礦體主要賦存於白系火山巖地層第二巖性單元的黃鐵絹英巖凝灰巖和第三巖性單元英安質疑灰巖中,上述巖石既是賦礦圍巖又是礦體。
  12. The plant body resembled a fern and did not produce flowers, the seeds developing from megasporangia borne on the margins of the fronds

    在石炭紀該種植物生長繁茂,到白紀基本滅絕,目前僅保留有石植物。
  13. Fifty - one and nineteen compounds were detected respectively from the volatile extracts of the fossils from miocene leaves of metasequoia glyptostroboides and early cretaceous seed cone of pityostrobus spp. by gas chromatography - mass spectrometry ( gc - ms ) analysis

    摘要採用氣相色譜質譜聯用分析技術從中新世水杉葉片和白紀松型球果兩種裸子植物石中分別鑒定了51個和19個揮發性成分,類型涉及烷烴、烷烯、烷醇、長鏈脂肪酸及其酯、鄰苯二甲酸酯、菇類和芳香族合物。
  14. Geochemistry of early cretaceous alkaline rhyolites from hulun lake, daxing ' anling and its tectonic implications

    呼倫湖早白世堿性流紋巖的地球學特徵及其意義
  15. Yanqi basin is stituated between tarim basin and tarpan - harmi basin. its petrolenm system underwent the formation and destruction during jurassic - cretaceous, the activation and reconstruction during tertiary - quaternary

    焉耆盆地位於塔里木盆地和吐哈盆地之間,其含油氣系統經歷了侏羅紀-白紀的形成與破壞階段和第三紀-第四紀的活與再建階段。
  16. 4. combined with the analysis of the hydrocarbon - generation history, hydrocarbon maturity, fluid inclusions, authigenic illites isotopes chronology and trap forming history, it affirms that jurassic reservoirs formed in three phases : the first in the late jurassic, which was the primary pool - forming phase, the second in the telophase of jurassic to cretaceous, which was the adjusting - destroying phase, the third in tertiary, which was the secondary phase

    4 、採用烴源巖生烴史、油氣成熟度、流體包裹體、儲層自生伊利石同位素年代學和圈閉演史綜合方法,確認焉耆盆地侏羅系油氣藏具有三期成藏的特點,第一期發生在侏羅紀晚期,是盆地的主要成藏期,第二期為侏羅紀末至白紀的油氣藏破壞、調整和再分配期,第三期發生在第三紀,是盆地的次要成藏期。
  17. The upper cretaceous and paleogene are of continental sediments in henan province, and the boundary between them considered to be unconformable or disconformable because of the very difference in sedimentation and biological assemblages

    摘要河南省上白統與古近系均為陸相沉積,在全省范圍內,兩者間呈假整合或不整合接觸,在沉積特徵上顯示出較大的差異,在古生物群的演方面,也各自具有不同的特色。
  18. The analyses of the sedimentary facies, rock geochemistry and reformation after the sedimentation from the upper cretaceous quantou formation to nenjiang formation indicate that the beneficial sand - bodies of the uranium deposit are mainly quantou formation ' s braided channel and qingshankou formation ' s delta sandstone types

    摘要從上白統泉頭組嫩江組沉積相展布、巖石地球學及沉積期后改造作用分析入手,闡明了研究區有利鈾成礦砂體主要為泉頭組的辮狀河與青山口組的三角洲砂體。
  19. A new type of dinosaur tracks from lower cretaceous of chabu, otog qi, inner mongolia

    內蒙古查布地區下白統巨齒龍足印
  20. It could be divided into six paleogeotemperature evolution stages from early cretaceous to recent based on the result of apatite fission - tracks analysis ; subsidence - buried history analysis shows that chagan experienced fault depression stage during early cretaceous bayingebi - suhongtu period, transional stage from fault depression to sag in yingen period, and sag stage since wulansuhai stage

    磷灰石裂變徑跡模擬分析結果認為早白世至今大致可分為6個古地溫演階段;沉降?埋藏史模擬揭示查干凹陷經歷了早白世巴音戈壁?蘇紅圖期的斷陷期、銀根期的斷?坳陷轉期和晚白世烏蘭蘇海期以來的坳陷期。
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