演化育生物 的英文怎麼說

中文拼音 [yǎnhuàyùshēngwù]
演化育生物 英文
evolutionary developmental biology
  • 演 : 動詞1 （演變; 演化） develop; evolve 2 （發揮） deduce; elaborate 3 （依照程式練習或計算） drill;...
  • 育 : 育動詞1. （生育） give birth to 2. （養活; 培育） rear; raise; bring up 3. （教育） educate
  • 生 : 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;...
  • 物 : 名詞1 （東西） thing; matter; object 2 （指自己以外的人或與己相對的環境） other people; the outsi...
  • 演化 : evolution
  • 生物 : living things; living beings; organisms; bios （pl bioi bioses）; biont; thing; life生物材料 biol...
  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、沉積儲層、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，沉積了巨厚的新生代地層，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，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。
  2. In 1999 from oneself started an undertaking until now, firstexperiences has started an undertaking, the skill market trains, really holds the management, the teaching management process, throughunceasingly charged the study, sums up experience, the union practicepromotion theoretical level, is the cosmetology profession and thecorrelation profession raise image design synthesizes the talentedperson thousand people, and was 30 enterprises successes plans theenterprise image, the market marketing brand, the staff etiquette, thequality, skill training ; and establishes the consummation educationalmodel, the educational administration management for the correlationprofession teaching unit, promotes the teachers level, to enhance thefresh source quantity : develops the new curriculum, like - - - " high - quality beautiful armor ", " improves looks beautiful releaseindustry mda management management ", " shanghai vocational educationfilm and television puts on make - up ", " color consultant ", " thecosmetology putting on make - up industry practical fine arts ", " practical human body colored drawing on pottery and beautiful armordesign ", " image design and psychoanalysis ", " image design andaccompaniment shopping ", " image design psychology consultation ", " advertisement animation drawing ", " fashion puts on make - up modelling " and so on, the compilation teaches document 22

    1999年從自我創業至今，首先經歷了創業、技能市場演練、實操經營、教學管理的過程，通過不斷充電學習、總結經驗、結合實踐提升理論水平，為美容行業及相關行業培養形象設計綜合人才千餘人，並為30餘家企業成功策劃企業形象、市場營銷品牌、員工禮儀、素質、技能培訓；並為相關行業教學單位創立完善教學模式、教務管理、提升師資水平、提高生源數量：開發新課程，如- - - 《高級美甲》 、 《美容美發行業mda經營管理》 、 《上海市職業教育影視化妝》 、 《色彩顧問》 、 《美容化妝業實用美術》 、 《實用人體彩繪及美甲圖案》 、 《形象設計與精神分析》 、 《形象設計與陪同購物》 、 《形象設計心理咨詢》 、 《廣告動漫繪畫》 、 《時尚化妝造型》等，編寫教案22本。
  3. In low - lying area, dark - colored mudstones have been developed, the organic matter richness are increased, the kerogen type is better and in matural stage, so it has better oil source bases

    窪陷內暗色泥巖發育，有機質豐度較高，乾酪根類型較好，處于成熟演化階段，具有較好的生油物質基礎。
  4. There are distributed a great number of cenozoic basalts and mantle derived xenoliths in north china and south china. for understanding the materials constitutes, evolution, mantle metasomatism, and inhomogeneity of the lower crust and upper mantle, there is a must of doing some research on these host basalts and the xenoliths

    華北、華南地區發育大量新生代玄武巖及幔源包體，對其進行研究，有利於進一步深入了解下地殼和上地幔的物質組成、演化、地幔交代和不均一性以及地球物理反演結果的可靠性等。
  5. Through field investigation, microscopic study, x - ray phase analysis and mineral infrared spectrum analysis, the authors determine the laumontitization had occurred widely in the axi gold field. according to the development of laumontitization and its relationship to mineralization, authors reveal that the laumontitization appeared mainly at the top and periphery to ore - bodies. it befallen at the edge of the geothermal fluid system or happened in the late stage of geothermal fluid system evolution, hence can be assigned as an indicator to prospect for epithermal gold deposit. the fluid causing laumontitization in the axi gold deposit is similar to those causing hot spring type gold deposit or in modern geothermal field. the fluidization of the axi gold deposit happened in carboniferous, showing the west tianshan is a good district for epithermal gold mineralization and preservation. so west tianshan is prospecting for exploring epithermal gold deposit

    通過野外考察顯微鏡下薄片鑒定x射線物相分析和礦物紅外光譜等研究，確定了阿希金礦濁沸石化的普遍存在根據濁沸石化發生的規律及其與礦床形成的關系，確定濁沸石化主要見于礦體的上部和外圍，發育在地熱流體系統的邊緣和演化晚期，可作為尋找淺成低溫熱液型金礦的標志之一。導致阿希金礦濁沸石化的流體性質與熱泉型金礦成礦流體和現代地熱田類似，流體作用發生在石炭紀，證明西天山地區具有良好的淺成低溫熱液型金礦的形成和保存環境，因此找礦前景較好。
  6. The development of reefs was controlled by the tectonic setting, sea - level movement, paleogeographic environment and evolution of reef - forming organisms

    生物礁的發育受構造作用、海平面變化及古地理環境控制，同時也受造礁生物興衰演化的控制。
  7. Therefore, the study of corporate organizational structural evolution is of vital importance to comprehension and interpretation of evolution for enterprises themselves and the whole economic system. focused on the study of corporate organizational structure and based on evolutional biology, complicated systematic theory, evolutional economics and organizational ecology, this thesis elaborates on the process, influencing factors and mechanism of corporate organizational structure evolution as well as the correlations of such evolution between corporate development and enterprise ecology succession. 1. this thesis comes up with four assumptions key to the study and defines corporate organizational structure

    本論文以企業組織結構進化現象作為主要研究對象，在進化生物學、復雜系統理論、進化經濟學和組織生態學等理論研究的基礎上，對企業組織結構進化的歷程、影響因素、進化機制，以及企業組織結構進化與企業成長發育和企業生態演替之間的相互關系展開了系統的討論: 1 .在提出四個關鍵的研究假設前提后，本文對企業組織結構進行了界定。
  8. During my master " degree investigation, i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts, the eastern yanshan, and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution, volcanism and tectonism. then i summarized the mesozoic basin development and the coupling characters of basin and mountain. the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic, the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous

    在野外典型路線調查的基礎上，對燕山地區東段承德、平泉地區的中生代盆地中發育的粗碎屑沉積層，進行了系統的物源分析與古流測定，並在此基礎上重點剖析了盆地的發育、火山活動、構造變動三者之間的關系，總結了本區中生代盆地發育規律及盆山耦合特徵，並將盆山演化劃分為：三疊紀?早侏羅紀的構造擠壓隆升與撓曲盆地發育階段階段，中晚侏羅紀的構造擠壓?火山活動與類前陸盆地發育階段，早白堊世的拉張斷陷盆地發育階段。
  9. Based on the direction of sources and the ratios of sandstone to formation of sedimentary rocks, together with the sedimentary structures and textures, paleocurrent direction and the characteristics of paleontology, etc., the planimetric maps of sedimentary facies of each stages in the studied area are compiled in order to recognized the extension of dominant facies and the evlotionary history of sedimentary environment, hi the stage of benxi and taiyuan, lagoon - tidal flat sediments are widespread in the area, and the deposits of estuary, lagoon and small delta in the northwest margin of ordos

    以物源方向和沉積巖砂地比值為基礎，結合沉積結構構造、古水流方向及古生物特徵等，編制了研究區各期次的沉積相平面圖，以識別優勢相展布和沉積環境演化。本溪期和太原期研究區瀉湖?潮坪沉積分佈廣泛，西北緣發育河口灣、瀉湖及小型三角洲沉積。
  10. The red tourism ' thrive is people ' s increases increasingly of spirit cultural the objective demand of the life, and it is also the inevitable request of the construction to have chinese special features socialism a forerunner culture. it puts education in touring and playing. it not only caters to the special needs of a part tourism market and enrichs the tourism industry, but also brings considerable economic income and promotes the development of the economy for the old revolution areas

    近年來，國內紅色旅遊悄然興起並迅速升溫，它是從有組織的革命傳統教育演化而成的新型旅遊產品，是革命傳統教育與旅遊產業相結合的產物，紅色旅遊的興起是人民群眾日益增長的精神文化生活的客觀需要，是建設有中國特色社會主義先進文化的必然要求。
  11. Transport of suspended matter ( sm ) on east china sea ( ecs ) continental shelf is very important for the development of continental physiognomy and its environment et al. the study of sm on ecs shelf is presently recognized as a front study in marine geology

    東海陸架懸浮體的輸送關繫到陸架地質地貌的發育和演化、陸架生態環境和陸架邊緣物質交換等方面。東海陸架懸浮體問題一直是學者們所關注的問題之一。
  12. By comparing the numerical results of water infiltration with air and without air, it is shown that the method in this paper is more effective for solving problems of water infiltration in unsaturated soil. in this paper the forming process of oil - bearing basin is the main research object and the mathematic model of geology is built, in order to simulate the dynamic forming process of stratums especially oil - bearing stratum in geology history in the time and space concept, further to investigate the history of petroleum forming, transmitting, accumulating and predict the distributing rule and scope of petroleum, and offer an rapid, quantitative, exact, general choice for the researcher of petroleum geology. with denudation, poor - compactness and sedimentation hiatus, the stratum relations of sedimentation section is judged, and the ancient thickness and pressure of stratum layer are recovered by the inversion method of back stripping. the numerical simulation algorithm of recovery of geological history is also given

    為了利用現代化的計算技術再現含油氣盆地的地史演化發育過程，以便進一步定量化研究油氣的生成、運移和聚集的歷史以及預測油氣分佈規律、分佈范圍，為石油地質學家提供一個快速、準確、定量、綜合的研究手段，本文就含油氣盆地的地史演化發育過程為主要研究對象，建立了數學地質模型，運用優化理論與演算法，在考慮了剝蝕、欠壓實、沉積間斷等地質現象的情況下，採用回剝反演法，應用鉆井、測井、地震等方法獲得的地層物性資料，判別沉積剖面中地層的接觸關系，恢復地層的古厚度、古壓力，構造了地史恢復的數值模擬方法。
  13. The origin and development of stone forest has attracted many karst researchers home and abroad, and they have done some macroscopical and microscopical studies on stone forest in terms of such conditions for its development as geology, climate, hydrological process, sub - soil corrosion, geomorphological types, history of development, paleo - geographical enviroment and biological effects etc, and put forward some development models, however, most of the studies just pay their attention to some single aspects of the problem

    石林的成因及發育演化問題引起了國內外喀斯特學者的關注，他們從地質、氣候、構造、水文過程、土下溶蝕過程、地貌成因類型、發育年代、發育歷史和古地理環境以及微形態的生物作用過程等方面對石林的形成發育進行了宏觀和微觀的研究，並提出了相應的發育演化模式，但多側重於單一方面的研究。
  14. Evolutionary developmental biology

    演化發育生物學
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