新生層 的英文怎麼說

中文拼音 [xīnshēngcéng]
新生層 英文
cambium
  • : Ⅰ形容詞1 (剛出現的或剛經驗到的) new; fresh; novel; up to date 2 (沒有用過的) unused; new 3 (...
  • : Ⅰ動詞1 (生育; 生殖) give birth to; bear 2 (出生) be born 3 (生長) grow 4 (生存; 活) live;...
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • 新生 : 1 (剛產生的) newborn; newly born 2 (新生命) new life; rebirth; regeneration; a new lease of [...
  1. Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock

    摘要以現有資料為基礎,通過對區域構造、沉積儲、烴源巖特徵等基礎石油地質條件研究,認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化,沉積了巨厚的代地,自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系,區域上存在始統、漸統和中統3套烴源巖,前代基巖潛山、漸統砂巖、中物礁3套儲,區域蓋為上統和更統淺海半深海相泥巖。
  2. Authigenic minerals and their occurrence in the meso - cainozoic reservoir sandstones were observed and analyzed by optical microscope, sem, epma and xrd

    採用光學顯微鏡、掃描電鏡、電子探針及x射線衍射觀察分析了塔里木盆地中界儲砂巖自礦物及其在巖石中的產狀。
  3. There is a north - north - east negative anomaly belt of aerial magnetism in the middle - east part of the basin, which could be displayed by the aerial magnetism of commutative field, upwardly continuation, lvt in earthquakes, the experimentation of granite liquation ( demagnetization ), the distribution of neozoic era volcanic rock, earthquake, hot spring and ground feature. the anomaly shows the blocking in east - west direction, and it is also associated with intense activity of deep heat interaction and the development of the crust - mantle mixed layer in the north qiangtang

    從區域航磁、向上延拓、地震低速、花崗巖熔融(退磁)實驗、代火山巖的分佈、地震、溫泉、地貌等發現,盆地中東部存在一北北東向航磁負異常帶,既顯示出東西分塊,也與北羌塘深部熱力作用強烈活動、發育「殼幔混合」有聯系。
  4. In a series of 30 cases of retinitis pigmentosa, pigment epithelial alterations included mottling of the macula in 8 eyes ( 13. 3 % ), bull ' s - eye pattern in 24 eyes ( 40 % ) and atrophy or hypopigmentation in 56 eyes ( 93. 3 % ) ; macular edema with retinal thickening was present in 30 eyes ( 50 % ), cystoid macular edema in 18 eyes ( 30 % ) ; broadening or loss of foveal reflex was present in 60 eyes ( 100 % ), preretinal membrane noticed in 58 eyes ( 96. 7 % ) and macular hemorrhage in one eye ( 1. 7 % )

    摘要對網膜色素變性癥的病例30例60眼探討其黃斑部病灶的情形,網膜色素上皮變化中的雜色斑點病變見於8眼,頻率為13 . 3 % ,牛眼樣病灶見於24眼( 40 % ) ,網膜脫色素病灶為56眼( 93 . 3 % ) ;黃斑部浮腫之網膜增厚為30眼( 50 % ) ,類囊胞浮腫為18眼( 30 % ) ;其它變化包括中心窩反射消失或增寬為60眼( 100 % ) ,網膜前纖維膜為58眼( 96 . 7 % ) ,黃斑部出血和疑似網膜下血管各為1眼( 1 . 7 % ) 。
  5. In contrast, the expression levels were low in diencephalon and brainstem in both newborn and adult mice. the cerebellum was the only area that differed significantly from the rest of the samples, with a higher expression in newborn mice, and a much lower expression in adult mice

    原位雜交分析顯示鼠小腦中, 3galt - 1在蒲肯野細胞和顆粒細胞中有強表達,而在成年鼠小腦中, 2000級博士學位論文p3galt一1在顆粒細胞的表達基本消失,這可能是p3galt一1在小腦發育前後表達差異的原因。
  6. However geological information is fully recorded in the remote sensing image, which made it possible for the choosing of this area as a dissection point to extract complex structural information of orogenic belt in west china. taking fully advantage of multi - band image richly bearing concealed geological information in combination with remote sensing analysis and structure analysis, to anatomy the supracrustal composition and structure of orogenic belt with the regional linear structures and their partitioned block and schistous geological masses as the macro - frame ( in corresponding to structure units and structure segments ) and with the rock masses, structure - rock assemblages, line - featured and belt - featured structures as well as penetrative and non - penetrative foliation ( primary stratum and trans position layering ) and folds as the texture and structure elements. the methods of how to distinguish granulite > ductile - shear zone, imposed fold, different deformed belts -

    因而,本文選擇這一地區作為我國西部地區從遙感圖像上提取造山帶復雜結構構造信息的解剖區,充分利用遙感圖像多波段反映物質屬性的特點和圖像處理提取隱含信息的優勢,採用遙感解析?構造解析相結合的研究方法,以區域線狀構造及由它劃分的塊狀、片狀地質體為宏觀骨架(對應于構造解析劃分的構造單元、構造均勻區段) ,以地質體中的巖石巖體、構造巖石組合,線狀、帶狀構造,透入性、非透入性面狀(原始理、面理)和褶皺等構造作為用於解析的結構構造要素,進行造山帶表殼組成和結構構造解析研究。
  7. The more accurate localization of 3galt - l mrna expression in mouse brain as studied by in situ hybridization was in good agreement with the general expression pattern seen with northern blot hybridization. in newborn mice, the dense granular layer and the purkinje cell showed a strong signal

    我們發現在小腦中1型鏈結構的變化與邵galt一1的表達變化基本一致:在鼠小腦中, 1型鏈結構在蒲肯野細胞和顆粒細胞中都有表達,而在成年鼠小腦中, 1型鏈結構僅在蒲肯野細胞中表達。
  8. They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill. we mark off five kinds of buried hill belts. they include three different kinds of trap on the basis of the cause of trap formation

    本次研究在重認識濟陽坳陷區域構造背景的基礎上,將濟陽坳陷古界潛山的形成過程分為四個階段,即古代早中代?穩定沉降?隆升?輕微褶皺變形及逆斷發育階段、中代?初步斷陷階段?塊斷期、代早期?斷拗階段?塊斷潛山形成期以及代晚期?坳陷階段?潛山定型期。
  9. “ salt ” bath features super moisturizing energy and can instantly warm the body, promote metabolism and blood circulation, intensively clean skin, remove aged horniness and make skin moist and supple

    「鹽」沐浴具有超強保濕潤澤能量,能使身體快速溫熱,提高陳代謝,促進血液循環,在洗浴同時能深潔凈肌膚,將體內的老化角質排出體內,維持肌膚柔潤如同
  10. The strata of the region are divided into two structural layers : the basement rock consisting of metamorphic rock and cover layer of mesozoic and neozoic sedimentary rock.

    將本區的地劃分為兩個構造:既變質巖系構成的基底構造;中代、代的沉積巖系構成的蓋構造
  11. ( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian, late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic. structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave. most traps in the area formed or typed at last in the himalayan episode, dispersed on the north and south belts

    ( 4 )研究區構造與地不整合圈閉的形成和發育受志留-泥盆紀、晚二疊世-第三紀、漸世-第四紀三個擠壓階段的控制;早古代主要發育非構造圈閉和復合圈閉,晚古代和代則主要發育構造圈閉:構造圈閉主要發育在南北兩帶上,其次為中帶;非構造圈閉主要發育在和田凹陷以北的地區;研究區內大多數圈閉是喜山期形成或最終定型的,在南北兩帶都有分佈,而海西期圈閉主要分佈於研究區中帶瑪南構造帶處。
  12. The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang, which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw, came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin, i. e. the strike - slip and stretch processes of baigezhuang fault

    同時,用三維地震資料進行區域構造解釋分析,論述了柏各莊地區的構造樣式,是中代渤海灣裂谷盆地的幕斷陷發育階段,同時由於盆地內凸起邊界?柏各莊斷的走滑兼伸展作用,使柏各莊凸起的中界形成壘、塹斷塊群構造樣式,發育一系列ne ( nee )向,傾向nw或sw的正斷
  13. Jiyang depression is a field where nonhydrocarbon is rich. these resources have close relation with the activities of the volcanos. at the same time, the activities of volcanos have deep contact with the activities of the faults. the growth of the faults in jiyang depression is great. by the research of the index number of the faults growth and the other researches, nw direction faults are the most ones in mesozoic, nw and ne and approximately ew directions all exist in cenozoic. the above reflects the whole geotectonic background that sinistral shearing stress field exists in mesozoic, but dextral shearing stress field exists in cenozoic

    這些氣藏與火山活動有密切的成關系,同時火山活動與斷裂活動也有密切的關系。濟陽坳陷內斷裂活動極為發育,通過斷長指數等的分析,推斷中代斷裂以北西向為主,代則兼有北西向北東向和近東西向的斷裂,上述斷裂發育特徵反映了該區的大地構造背景,在中代是左旋的剪切應力場,在代則是右旋的剪切應力場。
  14. The communication model is a twp - tier architecture, the main function of superstratum ( name server ) is tracing the domain which target agent belong to presently. the main function of substrate ( domain - inside tracing machine ) is the message transfer and denominating the new created agent

    本文所提的通信模型分為了兩結構,上的名字服務器主要提供按名字追蹤目標agent所屬域的功能,下的域內追蹤器完成消息轉發及為agent命名的功能。
  15. Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences. the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )

    通過研究有以下成果及認識:鄂爾多斯盆地及其周緣地區沉積蓋可劃分為五大構造序,盆地的形成和演化分為六大構造階段:太古代至古元古代基底形成階段、中元古代克拉通內裂陷槽或坳拉槽演化階段、震旦紀?早古代華北陸表海盆演化階段、晚古代?早中代華北克拉通坳陷演化階段、中代中晚期大鄂爾多斯內陸盆地演化階段及獨立鄂爾多斯盆地的形成、代周緣斷陷盆地演化階段。
  16. Filling sections of mesozoic - cenozoic tectonically active basins in china can generally be divided into five ordered, correlatable sequence stratigraphic units

    摘要中國中、代構造相對活動的斷陷或陸內前陸盆地充填序列一般可劃分出5個級別具有地對比意義的序地單元。
  17. The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep. under the background of indian plate subducting under asia - europe plate, bachu forebulge was greatly affected by the development of southwest depression and awati depression. almost all of its structure reversed, and as a result of it, both of its south and north boundary migrated. according to its evolution history and its feature, the authors tentatively use both - side migration model to interpret the evolution of compound forebulge. since triassic, almost all the spheres above lithosphere synchronously became flexure. because transpressional stress field became increasingly strong, bachu forebulge continued uplifting and big faults formed. then, bachu uplift, as a whole, slipped upward along those big faults and showed migrating toward thrust zone in plane. in tectonic tranquility, the lithosphere bounded back and in consequence of it, bachu uplift slipped down and showed migration toward craton, at that moment negative inversion structures developed. while the forebulge migrated toward its south and north foredeep, it was very possible that locally extensional stress appeared in the forebulge

    在印度板塊向歐亞板塊俯沖的大背景下,巴楚前緣斷隆受西南坳陷和阿瓦提凹陷的影響,代時構造體制發反轉,邊界向南北遷移。根據其發育過程特徵,作者用復合前緣隆起兩端遷移模式對復合前緣隆起獨特的構造發育史進行了解釋:即三疊紀以來巖石圈各圈同步撓曲變形。隨著擠壓應力場的增大,巴楚隆起在撓曲基礎上不斷抬升,形成幾條大型斷裂帶。
  18. Human fossil teeth newly discovered in nanshan cave of fusui, guangxi

    臨夏盆地的代地及其哺乳動物化石證據
  19. According to the analysis of the structure deformation variant direction the structure superposition during late period, and the tectonic stress field and deformation variant field, the cover extended nearly sn direction in early stage ( d - c ), maybe changed the direction in pernian ( especial the late permian ), and developed some new half - graben along sn direction except the succession activity at great fault zone. the direction of compression deformation variant, however, was nearly sn direction in indo - chinese epoch, ne - sw direction in early yanshan movement epoch, nne - ssw direction in late yanshan movement epoch, and transformed from ew to sn direction in himalayan movement epoch

    根據不同構造中變形方向及後期構造疊加的分析,對本區的構造應力場及變形場進行了探討,本區蓋早期階段( d - c )為近南北向的伸展拉張,二疊紀(特別是晚二疊世)的伸展方向可能發了改變,除在各斷裂帶繼承性活動外,沿南北方向又了一些半地塹。而在擠壓變形時,印支期主要為近南北向擠壓,燕山早期為nw - se向擠壓,燕山晚期為nne - ssw向擠壓,而喜山運動可能經歷了從ew向向sn向方向擠壓的轉變。
  20. According to the synthetically study of remnant stratum list, sediment system. character of sediment filling, comeback of archetypal basin and feature of tectonic deformation, santanghu basin passed through four formation and evolution phases : ( 1 ) formation and evolution of basin ' s basement ; ( 2 ) formation and evolution of fault - fold to depression basin in permian ; ( 3 ) formation and evolution of depression basin in triassic - jurassic - cretaceous ; (

    依據三塘湖盆地殘餘地序列、沉積體系、沉積充填特徵和原型盆地恢復,以及不同構造的構造變形特徵的綜合研究分析,認為三塘湖盆地經歷了如下四個發展演化階段:前二疊紀盆地基底發展演化階段;二疊紀斷陷-拗陷盆地發展演化階段; :三疊-侏羅-白堊紀拗陷盆地發展演化階段;第三-第四系代盆地發展演化階段。
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