裂內的 的英文怎麼說

中文拼音 [liènèide]
裂內的 英文
intrafissural
  • : 裂動詞[方言] (東西的兩部分向兩旁分開) open
  • : 名詞1. (內部; 里頭; 里邊) inner; inside; within 2. (妻子或妻子的親屬) one's wife or her relatives 3. (姓氏) a surname
  • : 4次方是 The fourth power of 2 is direction
  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,對該區縫性儲集層類型識別、孔滲特徵測井地質解釋以及儲層發育和分佈規律進行深入研究便成為本文研究出發點。為此,本文從測井地質角度,針對當前縫性儲層測井地質解釋與評價現狀,在綜合分析當前國外儲層分形分維研究成果基礎上,利用分形分維方法和技術,通過對archie測井解釋模型中m指數、 n指數分形分維特性深入淺出論述以及縫性儲層段測井曲線分維d _ ( fa )與m指數理論推導,根據縫性儲層測井曲線形態分維值地球物理意義? ?曲線變化越復雜,則其分維值d _ ( fa )越大、縫孔隙空間結構越復雜、縫孔隙空間結構指數m值越高等特徵,提出了改進基於盒維數測井曲線網格覆蓋法,編程計算了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區塊縫油藏進行應用研究,效果十分理想: 1將計算得到可變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區塊下白堊統縫性儲層類型識別。
  2. Embryological studies reveal that megaspore and such cells as egg, synergid and antipodals in mature embryo sac initiate the division of forming haploid plants through embryogenesis or callus formation

    胚胎學觀察揭示大孢子與胚囊卵細胞、助細胞和反足細胞均有可能在培養中啟動分,通過胚狀體或愈傷組織形成單倍體植株。
  3. Any place within the fault zone could have breakage.

    斷層帶任何地方都會有破
  4. The total amatoxins concentration from carpophore of a. fuliginea collected in different development stages were studied. the result showed that the highest content of total amatoxins ( 23793. 3 g / g ) was found in the carpophore with the cap free from veil but the gill concealed by veil and, the lowest content of total amatoxins ( 4674

    灰花紋鵝膏菌不同發育時期子實體毒素分析表明:以菌蓋尚未充分展開,菌幕即將破毒素含量最高( 23793 . 3 g g ) ,在凋萎時急劇降低( 4674 . 9 g g ) ,只有最高時19 . 65 。
  5. The fault controlled the magmatism and metallization relevant to the contact zone, and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene. the fault zone deformed right - laterally under ne - sw striking transtention, and new joints zone was produced at the end of the two main faults because of local stress concentration. the fault produced inchoative cataclastic rocks, and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks, which was during the himalayan movement

    其後繼承性活動在斷形成碎程度最強達到碎巖系列構造巖,變形帶兩側發育兩組典型共軛剪節理;第二次在晚白堊世?始新世,斷在北東?南西向近水平擠壓作用下右行張扭性活動,斷帶兩主斷在斜列重疊端部由於局部應力集中進一步擴展形成節理帶,而斷在巖體區也發育兩組典型共軛剪節理,斷形成初碎巖為主構造巖;第三次是喜山期以西側抬升、東側下降強烈升降為主活動,在基巖中,主斷層兩側圍巖出現微破
  6. The dimensions of rupture zones in various island areas appear to be related to the extent of prominent deep-sea benches.

    各種島嶼大小似乎與突出深海階地范圍有關。
  7. On the basis of detailed field work and structural analysis, this paper presents a new geometrical and kinematic data that reveal the staictural characteristics of qinglong fault zone. this fault zone is composed of numerical ew faults with an arrangement of dextral step pattern in the western part, and consists of maquanzi - datun fault and tumenzi - mingshui fault in the eastern part

    本文通過較為詳細野外調查和室研究,並結合前人研究資料,以構造解析為指導思想,對斷幾何學、運動學特徵進行了研究:青龍斷帶是由一系列近東西向斷層組合而成,斷帶西段呈明顯右行右列式分佈,東段主要有馬圈子?大屯斷和土門子?明水斷組成。
  8. It is believed that three northeast - striking dextral slip fault zones, i. e. the baxian - shulu - handan fault zone, the huanghua - dezhou - dongming fault zone, and the linyi - huanghekou fault zone, are the result of the tectonic transform of paleogene extending to neogene - quaternary laterally slipping of north china plain rift systems, which extend along the central axis of rifts and accord with the quaternary centers of subsidence as the main seismic structures within the rifts

    認為壩縣束鹿邯鄲斷帶、唐山河間磁縣斷帶和黃驊德州東明斷帶3條北東向右旋走滑斷帶為華北平原谷系從早第三紀伸展拉張作用進入晚第三紀第四紀走滑剪切拉張作用產物,這3條斷帶分別位於3個北東向坳陷帶中部,並構成了第四紀沉降中心,與營口濰坊斷帶起構成華北平原主要強震構造。
  9. The minerogenetic model of xikuangshan type copper deposit can be concluded that : in jinningian - chengjiangian, the activity of xiaojiang discordogenic fault form dextrorotation sub - structure in dongchuan ore area

    昆陽多數銅礦同位素成礦年齡多集中在9 . 0億6 . 5億年之間,屬于晉寧-澄江期,與rodina大陸解時限相當。
  10. The object pattern of this reconstruction is to substitute the formal one thing one right principle and the plane structure of real rights theory with the virtue principle and the solid structure, to separate the abstract real rights that indicate the attribution of the thing from the material real rights that indicate the content of the disposal, to acknowledge the phenomena of value split, intention split and effectiveness split, to abstract the general rules applied to the dominative power of property, to unify the domination of corporeal and incorporeal into the system of real rights

    物權理論結構必須重塑。重塑目標模式是用實質一物一權主義替代形式一物一權主義,用立體物權理論結構代替平面物權理論結構。將表示物歸屬抽象所有權與表示支配具體所有權分離,承認物權價值分、目、效力分現象,提煉出適用於財產支配權一般規則,將有體物和無體物支配統一到物權制度之中。
  11. We simply removed from the cracked endocarp with sterile tweezers.

    我們簡單地用消過毒鑷子從果皮中取出種子。
  12. Optimization of synthetic process of aqueous cationic etherifying agent

    新型清潔壓合成及性能研究
  13. It is the regional structure stress field formed in the processes of formation of the major faults of buried hills action on the graben that controlled the development of the fractures of sandstone of mesozoic of baigezhuang region

    正是壘塊上古潛山幕主要斷層形成過程中局部構造應力場,控制形成了柏各莊地區潛山中生界砂泥巖中發育。
  14. Yili basin is a independent unit of the yili - zhongtianshan micro plate, which is subject to the zhunger - kazakstan plate. it is a superimposed basin which formed on the basis of the folded pre - permian basement, underwent rifting and breaking in permian, depressing and uplifting and multiple deformation and reformation after permian

    伊犁盆地是準噶爾?哈薩克斯坦板塊一個次級構造單元?伊犁-中天山微板塊一個獨立單元,它是在前二疊紀褶皺基底基礎上,於二疊紀擴張、解(谷) ,經二疊紀后坳陷、隆升多期變形、改造而成復合型改造盆地。
  15. Laminar flow of foam fracturing fluid in fractures

    泡沫壓液在層流流動
  16. It ' s a kind of dead soft - rock with some special characteristics of muddiness, softenness, dehydrate and rift etc when it meet water. however, the articles about the socketed piles in this stratum had not been discovered

    昔格達組泥巖在四川境西昌、攀枝花地區分佈較為廣泛,該巖層具有遇水泥化、軟化和脫水開等特徵,屬極軟巖類。
  17. For information on nuclear fission and chain reaction in a nuclear reactor

    若你想了解核反應堆變及連鎖反應,請
  18. Thus the fracture likely initiated from fatigue sharpened cracks originating from slag and void in the plug welds.

    因此,斷可能是由於從塞焊焊縫焊渣和氣孔外形成尖銳疲勞紋而產生
  19. The spores are liberated by rupture of the sporangium wall

    當孢子囊壁破時可以將其孢子釋放出來。
  20. The sankeng geothermal field is located on the northeastern side of the wuchuan - sihui deep fault and in the sankeng synclinal karstic basin

    摘要廣東三坑地熱田位於吳川四會深大斷東北側,三坑向斜巖溶盆地
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