裂內的 的英文怎麼說
中文拼音 [liènèide]
裂內的
英文
intrafissural-
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。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內的卵細胞、助細胞和反足細胞均有可能在培養中啟動分裂,通過胚狀體或愈傷組織形成單倍體植株。Any place within the fault zone could have breakage.
斷層帶內的任何地方都會有破裂。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的子實體毒素分析表明:以菌蓋尚未充分展開,內菌幕即將破裂時的毒素含量最高( 23793 . 3 g g ) ,在凋萎時急劇降低( 4674 . 9 g g ) ,只有最高時的19 . 65 。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
其後的繼承性活動在斷裂帶內形成碎裂程度最強達到碎裂巖的碎裂巖系列構造巖,變形帶兩側發育兩組典型的共軛剪節理;第二次在晚白堊世?始新世,斷裂在北東?南西向近水平擠壓作用下右行張扭性活動,斷裂帶兩主斷裂在斜列重疊的端部由於局部應力集中進一步擴展形成節理帶,而斷裂在巖體區也發育兩組典型的共軛剪節理,斷裂內形成初碎裂巖為主的構造巖;第三次是喜山期以西側抬升、東側下降的強烈升降為主的活動,在基巖中,主斷層兩側圍巖出現微破裂。The dimensions of rupture zones in various island areas appear to be related to the extent of prominent deep-sea benches.
各種島嶼內斷裂帶的大小似乎與突出的深海階地的范圍有關。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
本文通過較為詳細的野外調查和室內研究,並結合前人的研究資料,以構造解析為指導思想,對斷裂帶的幾何學、運動學特徵進行了研究:青龍斷裂帶是由一系列近東西向的斷層組合而成,斷裂帶西段呈明顯的右行右列式分佈,東段主要有馬圈子?大屯斷裂和土門子?明水斷裂組成。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裂帶、唐山河間磁縣斷裂帶和黃驊德州東明斷裂帶3條北東向右旋走滑斷裂帶為華北平原裂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的產物,這3條斷裂帶分別位於3個北東向坳陷帶中部,並構成了第四紀沉降中心,與營口濰坊斷裂帶起構成華北平原內的主要強震構造。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
昆陽裂谷內的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大陸裂解時限相當。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。重塑的目標模式是用實質的一物一權主義替代形式的一物一權主義,用立體的物權理論結構代替平面的物權理論結構。將表示物的歸屬的抽象所有權與表示支配內容的具體所有權分離,承認物權的價值分裂、目的分裂、效力分裂的現象,提煉出適用於財產支配權的一般規則,將有體物和無體物的支配統一到物權制度之中。We simply removed from the cracked endocarp with sterile tweezers.
我們簡單地用消過毒的鑷子從裂開的內果皮中取出種子。Optimization of synthetic process of aqueous cationic etherifying agent
新型清潔壓裂液的室內合成及性能研究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
正是壘塊上古潛山內幕主要斷層形成過程中的局部構造應力場,控制形成了柏各莊地區潛山中生界砂泥巖中裂縫的發育。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?哈薩克斯坦板塊的一個次級構造單元?伊犁-中天山微板塊內的一個獨立單元,它是在前二疊紀褶皺基底的基礎上,於二疊紀擴張、裂解(谷) ,經二疊紀后的坳陷、隆升多期變形、改造而成的復合型改造盆地。Laminar flow of foam fracturing fluid in fractures
泡沫壓裂液在裂縫內的層流流動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內的西昌、攀枝花地區分佈較為廣泛,該巖層具有遇水泥化、軟化和脫水開裂等特徵,屬極軟巖類。For information on nuclear fission and chain reaction in a nuclear reactor
若你想了解核反應堆內的核裂變及連鎖反應,請Thus the fracture likely initiated from fatigue sharpened cracks originating from slag and void in the plug welds.
因此,斷裂可能是由於從塞焊焊縫內的焊渣和氣孔外形成的尖銳的疲勞裂紋而產生的。The spores are liberated by rupture of the sporangium wall
當孢子囊壁破裂時可以將其內的孢子釋放出來。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裂帶的東北側,三坑向斜巖溶盆地內。分享友人