白堊統 的英文怎麼說

中文拼音 [báiètǒng]
白堊統 英文
chalk
  • 白 : Ⅰ形容詞1 （似雪的顏色） white 2 （清楚; 明白; 弄明白） clear 3 （空的; 沒加他物的） pure; clear; ...
  • 堊 : Ⅰ名詞（白堊; 白土） chalkⅡ動詞[書面語] （用白堊塗飾） cover with chalk; chalk
  • 統 : Ⅰ名詞1 （事物間連續的關系） interconnected system 2 （衣服等的筒狀部分） any tube shaped part of ...
  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? ?曲線變化越復雜，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化的規律，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區塊下白堊統的裂縫性儲層的類型識別。
  2. ( 3 ) 6 the 3rd - order sequence have been identified in early cretaceous, the position of sequence is erected on 2 sets andesite

    （ 3 ）將下白堊統劃分為6個三級層序，指出本區兩層安山巖的層序位置。
  3. Upper cretaceous rudist bioherms in southwestern tarim

    塔里木盆地西南地區上白堊統生物丘
  4. The upper cretaceous jingzhushan formation in the biru basin, xizang consists of a succession of coarse - grained elastic rocks in the alluvial fan - fan delta depositional system, intercalated with intermediate - acidic volcanic rocks including dacite, andesite, quartz trachyandesite and rhyolite

    摘要上白堊統競柱山組為一套沖積扇扇三角洲沉積體系的粗碎屑巖，間夾由英安巖、安山巖、石英粗安巖和流紋巖組成的中酸性火山巖。
  5. 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

    摘要河南省上白堊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，在古生物群的演化方面，也各自具有不同的特色。
  6. 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

    摘要從上白堊統泉頭組嫩江組沉積相展布、巖石地球化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。
  7. A new type of dinosaur tracks from lower cretaceous of chabu, otog qi, inner mongolia

    內蒙古查布地區下白堊統巨齒龍足印化石
  8. Lower cretaceous bayingebi group had higher organic abundance, generating hydrocarbon intensity and hydrocarbon expulsion efficiency. there were petroleum migration and accumulation in three phases through the analysis of fluid inclusion

    下白堊統巴音戈壁組二段具有較高的有機質豐度、生烴強度和排烴效率，由流體包裹體分析查干凹陷存在三期油氣運聚史。
  9. The main conclusions are as follows ; firstly, under the influence of three phases of episodic activities, three two - order sequences is composed of three depositional cycles and three regional unconformities ; secondly, under the control of structure activities such as fault - block activities and the influence of three - order climate cycles and source recharge, lower cretaceous can be divided into six three - order sequence ; thirdly, because fault activities is weak and fault slope is gently, fan deltas exist in steep slopes in early and later stages and subaqueous fans exist and turbidite fans exist in troughs in middle stage

    主要的結論為：其一，受三期幕式活動影響，斷陷形成了3個大的沉積旋迴和3個區域不整合面，構成了下白堊統3個二級層序；其二，受斷陷內翹傾和塊斷等構造活動的控制，以及三級氣候旋迴和物源供給因素的影響，下白堊統劃分出6個三級層序；其三，在單斷斷陷湖盆中，湖泊階段的早、晚期由於凹陷邊界斷層活動較弱，斷面較緩，陡坡可以發育扇三角洲，在湖泊階段的中期主要為水下扇砂礫巖體，並在窪槽區發育濁積扇。
  10. Evolution and sequence stratigraphic framework of lower cretaceous in chagan depression

    查干凹陷下白堊統層序地層格架與演化
  11. The depositional character of zhuxiang formation in the basin reads as follows : a series of nne alluvial fan were formed along the fault. the half - deep lake to deep lake faces appeared by west side of the fault, towards the west the saucer lake faces, shore deposit and flood plain face appeared in proper order. the depositional center of lower cretaceous was formed in eastern part of the basin, and the depositional depth was pinch - out and thinning out from the east to the west

    盆地內下白堊統朱巷組沉積特徵表現為：沿郯廬斷裂帶呈北北東向廣泛發育了沖積扇體系，從近斷裂帶西側出現的半深湖-深湖相，向西依次為濱淺湖相到泛濫平原相的規律性分佈，沉積厚度由東向西尖滅、超覆，構成了明顯的東斷西超的盆地構造格局，表明下白堊統的沉積中心依然位於盆地東部。
  12. However, the reservoir porosity and permeability of lower cretaceous in erlian basin is better than that of yingen - ejinaqi basin

    但二連盆地下白堊統儲層的孔隙度和滲透率比銀根額濟納旗盆地要好得多。
  13. The types and characteristics of the sedimentary facies developed in pukou formation of upper cretaceous in huaiyin sag of yanfu depression are analyzed

    摘要對鹽阜坳陷淮陰凹陷上白堊統浦口組發育的沉積相類型及其特徵進行了分析。
  14. The sediment stratum in chagan depression is devised into tree supersedences. among them, lower cretaceous can be devised into eight sequences and twenty - two system tracts which have been studied in characteristics of sedimentary cycle, distribution and genetic analysis. after this study, formed mechanism, distribution model and evolvement of sequence have been put forward

    查干凹陷共劃分出3個超層序，研究目的層下白堊統劃分出8個層序， 22個體系域，並進行了層序地層格架的層序沉積旋迴特徵、層序展布特點和層序成因分析，提出了斷陷盆地層序的形成機制、層序地層分佈模式與演化模式。
  15. It points out the targets for next exploration in yingen - ejinaqi basin are the lithologic and stratigraphic as well as buried hill reservoirs ( volcanic rock and granite ) in the east, the jurassic and lower cretaceous as well as buried bill ( pre mesozoic granite ) reservoirs in the west

    提出了銀根額濟納旗盆地的下一步勘探方向：在東部，以巖性、地層、古潛山（火山巖或花崗巖）油藏為主：在西部，以侏羅系、下白堊統及古潛山（前中生界花崗巖）油藏為主。
  16. Sedimentary environments of submarine fan of the lower cretaceous in northern himalayas

    北喜馬拉雅地區下白堊統海底扇沉積環境
  17. On the basis of sequence stratigraphy analysis of bayindulan sag, wuliyasitai depression, jiergalangtu sag and saihantala sag, the integrated sequence stratigraphy section of lower cretaceous has been established and the vertical sequence of sandbodies distribution in three - order sequence has been concluded

    本文通過對巴音都蘭、烏里雅斯太、吉爾嘎朗圖和賽漢塔拉等凹陷層序地層分析，建立了二連盆地下白堊統層序地層綜合剖面，並總結了三級層序框架內砂體分佈的垂向序列。
  18. ( 6 ) deposition - seismic response is obvious, 17 series ( 3 types ) seismic facies have firstly been identificated in early cretaceous and from seismic facies to deposition facies has been finished

    （ 6 ）首次將下白堊統地震相劃分為三大類共17種地震相單元，並完成了由地震相沉積相轉相工作。
  19. With regard to distinguishing containing of the water and gas, the cretaceous is the difficult point on logging interpretation all the time in the majing of western of sichuan. it is mainly the diversity of the containing of gas and water is very difficult to distinguish. gas and water react very closely in the log

    對于含水含氣性識別，川西馬井地區下白堊統含氣性識別一直是測井解釋的難點，主要在於儲層含氣性差異分辨較困難，氣和水在測井曲線上的響應比較接近，過去解釋的部分氣層測試卻產水，常規的測井解釋方法很難將二者區分開。
  20. Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin - controlled faults, tanlu fault zone strike slip to develop the three nw - trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben. based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene. the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull - apart basin in cenozoic time. the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin - controlled faults in the different depresses in bohai basin. the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin

    根據中生界上侏羅統和下白堊統地層和控盆斷裂分佈分析，中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導致郯廬斷裂帶以西自北向南發育了3個北西向斷塹系，即北部的渤海斷塹系中部的濟陽斷塹系和南部的魯西南斷塹系。從區域資料綜合分析，渤海灣盆地的基本格局是早第三紀以來的新生代盆地格局。渤海灣盆地的形態構造和沉積特徵及熱流值分佈表明該盆地在新生代為拉分盆地。
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