始古生代 的英文怎麼說

中文拼音 [shǐgǔshēngdài]
始古生代 英文
eopaleozoic
  • 始 : Ⅰ名詞1 （最初; 起頭） beginning; start 2 （姓氏） a surname Ⅱ動詞（開始） start; begin Ⅲ副詞[書面...
  • 古 : Ⅰ名詞1 （古代） antiquity; ancientry 2 （先哲的遺典、道統） books or orthodoxies of ancient sages...
  • 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;...
  • 代 : Ⅰ動詞1 （代替） take the place of; be in place of 2 （代理） act on behalf of; acting Ⅱ名詞1 （歷...
  1. Because bai minority ' s economy was affected deeply by the mainland ' s han culture, cultivated the opened self - conscious national spirits for a long time ; been good at studying, imitating and innovating, furthermore had the national character and morals that looked up the wise, so it brought the advanced economic conformation whether in the ancientry or latter - day, speeded up the development of productivity, maked the dali bai minority situated the center station of the regional economic development, had the ability of deciding and imposing on the economic changes and economic relations that circumjacent nation area, historically introjected the extensive circulation of chinese economic development, and became a part of chinese economy

    白族經濟始終與白族發展歷史相伴生，歷史傳承下來的大量富有白族經濟特徵的民族經濟現象，至今仍然客觀真實地存在。由於深受中原漢文化的影響，使白族經濟在古代和近代，產生了先進的經濟形態，促進了生產力的發展，使大理白族經濟處于地區經濟發展的中心地位，具有決定和影響周邊民族地區的經濟變化與經濟關系的能力，歷史地融入中華民族經濟發展的大循環圈，成為中華民族經濟的一個組成部分。社會主義市場經濟體制的確立，對民族經濟的發展研究提出了嶄新的課題。
  2. Four tectonic evolution phases have been made out in this area. they are original crust formed in the archean - early proterozoic era, continental crust shearing in the middle - new proterozoic era, plate tectonic developed in sinian - triassic period and intracontinental orogeny in the middle cenozoic period

    將區內構造演化歸納為太古?早元古代原始地殼形成、中新元古代大陸地殼裂解、震旦?三疊紀板塊構造體制、中新生代陸內造山等四個演化階段。
  3. Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase

    查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元，其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成的陸緣或島弧褶皺帶，具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖的構造環境；燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶的增厚陸殼開始發生伸展垮塌的構造環境；早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。
  4. The principle of cyclic sedimentation applies to deposits dating from earliest paleozoic time to the holocene.

    旋迴沉積原理適用於始於最早的古生代迄至全新世的沉積物。
  5. The karst formation of phong nha - ke bang national park has evolved since the palaeozoic ( some 400 million years ago ) and so is the oldest major karst area in asia

    豐芽格邦國家公園的喀斯特地貌的形成是從古生代（大約40億年前）開始的，是亞洲最古老的喀斯特地貌。
  6. The mesozoic primary hydrocarbon accumulation has been heavily damaged by the denudations at latest middle jurassic and latest cretaceous and the faulting from paleocene to eocene

    中侏羅世末期、白奎紀末期的地層抬升剝蝕，以及古始新世的斷裂活動對中生代形成的原生油氣藏破壞作用明顯。
  7. Therefore, economic theory and actual costs is the most core economic activities, from the classical economists, until modern economists, management scientists to study the issue of production costs has never ceased

    所以，成本問題是經濟理論與實際經濟活動中最為核心的問題，從古典經濟學家開始，直到現代經濟學家、管理學家對生產成本問題的研究從來都沒有停止過。
  8. Through research, the organic matter of source rocks in carboniferous - permian coal measure strata began first hydrocarbon - generating in mesozoic, and the first hydrocarbon - filling took place. but, because of yanshan movement later, the carboniferous - permian strata rose, as a result, the first hydrocarbon - generating and reservoir - forming paused ; in early tertiary period, because carboniferous - permian strata dipping forward east originally turned into dipping forward west, the prototype of faulted block began to form gradually ; by the end of sha - 3 period of early tertiary, the paleogeotherm of carboniferous - permian strata exceed the mesozoic ' s temperature again, and accordingly, abundant hydrocarbon was generated and expulsed secondly. the trap continued to develop ; from the end of late tertiary to quaternary, the second hydrocarbon - generating and expulsing got to its peak, and the second reservoir - forming was over

    研究表明，本區石炭?二疊紀烴源巖在中生代發生一次生烴和排烴，並有油氣充注，后因燕山運動導致地層抬升，一次生烴和成藏過程中止；在早第三紀，原來東傾的地層變為西傾，斷塊圈閉開始具雛形；至早第三紀沙二末期，石炭?二疊系的大部分地層古地溫再次超過中生代一次生烴的溫度，開始二次生烴和排烴，圈閉持續發育；晚第三紀末?第四紀，二次生烴、排烴達到高峰，二次成藏完成。
  9. Thus, it can be clearly recognized that the global continents located at near equator and southern hemisphere, showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia, siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards, the amalgamation in north - south direction at the western parts of laurentia and gondwana, subducted the lapetus and rheic oceans, until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards, to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean, preserved the status of dispersion, gradually moving to northwards, showed the characteristics of range along north - south orientation, until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling, kunlun, qinling - dabie, jingshajiang and shaoxing - shiwandashan zones, thus the most part of chinese continental blocks amalgamated to eurasia continent

    由此可以清晰地看出，在古生代早期全球各大陸的主要部分都位於赤道附近及南半球，大致表現為沿緯度、呈東西向排列的特徵，中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間；隨著西伯利亞大陸的快速北移，在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合，亞皮特斯洋和里克洋的消亡，到古生代晚期形成統一的泛大陸；而岡瓦納大陸的東部（澳大利亞和印度等）則逐漸向南移動、離散，地殼張開，構成古特提斯洋；中國及鄰區的小陸塊群則一直處在古特提斯洋中，保持離散狀態，總體上緩慢地向北運移，並逐漸轉為近南北向的排列方式，石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞，使中國大陸地塊的大部分逐漸併入歐亞大陸。
  10. Cambrian : the beginning of the paleozoic era animals with hard - shells appeared in great numbers for the first time during the cambrian

    寒武紀：古生代的開始（距今5億1 ， 400萬年前） ，具有硬殼的生物在寒武紀第一次大量出現。
  11. Tian shan extends east - west in central asia, the tian shan range was formed in later paleozoic, and a few intramontan basins appeared in mesozoic. it uplifetd again in early miocene because of the north - south compression induced by the india - asia collision, so many active structures can be found in tian shan. active tectonics took actions during last ten thousands yeas, and surface traces of fault scarps, detached gullies and folds in alluvial deposit are apparent, so it is easy to distinguish them from other geological phenomema

    天山位於亞洲中部，天山造山帶形成於晚古生代，到中生代時，在天山內部形成了一些山間盆地，印度板塊在始新世向北與歐亞板塊碰撞，天山受南北向擠壓力的作用再度于早中新世隆起，由於板塊碰撞的持續進行，在天山山間及山前發育了許多的活動構造。
  12. Located at south gate of 798 art area, dashanzi, beijing, liana art space covers the exhibition room of 66 square meters, with simple decoration by keeping old building style, it achieves virtual results of classical and modern art

    青藤子藝術空間位於大山子798藝術區南門，展廳面積約66平方米，裝修風格簡潔通暢，保留了原來舊式工廠的一些原始風貌，與現代藝術作品形成強烈對比，古樸中體現藝術的獨創感覺，生動而深遂。
  13. Those two phases of conjugated shear joints are differ from each other in spatial distribution, which is a reflection of the spatial evolution of the fault zone. it can beinferredfrom the information about macrostructure, superimposed deformation of tectonites, paleotectonic stress field of joints and other related documents that there had been three stages of significant activity since zijingguan fault zone was activated. the first stage was about from middle juiassic to early cretaceous, when the fault zone activated left - laterally under nw - se striking transpression

    宏觀構造組合特徵、構造巖變形疊加信息、節理的古構造應力場信息及前人區域資料表明，紫荊關斷裂帶自古生代末開始活化以來有三次主要構造活動：第一次是中侏羅世?早白堊世，在北西?南東向近水平擠壓作用下，斷裂左行壓扭性活動，控制太行山地區巖漿巖帶及與其相關的接觸交代型礦床的形成。
  14. In ancient times artisans drew pictures of " door gods " to drive away evil spirits

    民俗風情年畫的始袍產生於上古時代。
  15. By studying the lithologjcal and mineral parameters ( pebbled elastics percent ratio, clastic maturation index, heavy crop stability factor ) of mesozoic sedimentary strata, the result shows that the northern boundary of present basin is near to the boundary of original basin and the moving distance of elastics is short, but the southern boundary of present basin is far from the boundary of original basin and the moving distance of elastics is long. the fades of northern basin are mainly delta fades and the fades of middle and southern basin are lacustrine fades

    通過對盆地中生代沉積地層中各種巖礦參數（碎屑巖含礫百分比、碎屑成熟度指數和重礦物穩定系數）分析和綜合研究認為，今盆地北部距離原始盆地沉積邊界較近，碎屑物搬運距離較短；南部距離盆地古沉積邊界較遠，沉積物搬運距離較遠；中生代盆地北部主要為三角洲沉積相，中南部為湖泊相沉積。
  16. The paper falls into six parts. the first chapter is the survery of the paper. the second chapter probe the origin of the eco - architecture, clarify the ancient habitation is the exhibition of the archetype of all kinds of architecture and reflect human ' s aboriginal life style. so, the ancient habitation is the oldest eco - architecture. the third chapter states that in the history of westen modern architecture, the ecological architectures in the early stage were associated with the climate conscious designs. with the reaearch on the ecological architecture which influenced by the green - movement after 1960 ' s, the forth chapter analyze it ' s background and course. the fifth chapter discuss the two types of westen eco - architecture after 1970 ' s : low - tech eco - architecture and high - tech eco - architecture, analyze the works of representative architects and point to the trend of the high - tech of the development of the westen eco - architecture

    第二章探尋了生態建築的緣起，闡明了古老的民居反映了人類最原始的生活方式，是所有建築的原型的實體表現，同時也是人類最古老的生態建築。第三章從發掘現代西方建築歷史上曾經出現過的部分注重生態的建築設計萌芽入手，指出早期的與注重生態的建築設計相關的研究表現為適應環境與氣候的建築設計。第四章針對60年代以後受綠色運動影響的注重生態的相關理論和實踐進行了剖析，分析其產生的背景和發展演變過程。
  17. Forty years ago, for example, palaeontologists thought that hominids, the group of primates that includes modern humans, had been distinct from other apes for some 25m years

    比如四十年前，古生物學家就認為原始人（包括現代人在內的靈長類群體）與大約2500萬年前的其它類人猿明顯不同。
  18. Ascertaining the paleocurrent direction of the mesozoic basin and reconstructing the paleogeography ; ( 4 ). deciding the material components and original structure sequences of the basin provenance, and coupling relationship between the sediments of the basin and geologic units of the provenance ; ( 6 ). establishing the mesozoic tectonic evolution history of the dabie orogenic belt and discussing the collisional mechanism of the belt

    主要研究內容包括：釐定大別山北緣地區中生代地層的年代格架；劃分巖相，確立沉積體系；確定中生代盆地古流向，恢復盆地的古地理；確定物源區物質組成、演繹物源區原始構造層序、建立盆地沉積物與物源區地質單元的耦合關系；根據沉積學以及區域地質研究，重塑大別山中生代構造演化歷史，探討大別山造山帶的碰撞成因機制。
  19. The research on the lithologjcal and mineral parameters and the sedimentary fades of different periods of mesozoic strata shows that the northern boundary of yanqi basin is almost the same, but great differences existed in the southwestern yanqi basin, that is, the sedimentary range of mesozoic original basin is more bigger than present basin

    中生代地層各種巖礦參數和各時代沉積相研究表明，今焉耆盆地北部與原始沉積邊界較為相近；西南和南部的邊界今古差異較大，即在中生代原始盆地沉積范圍要比今盆地范圍要廣。
  20. " amber is like a time capsule made and placed in the earth by nature herself, " said david federman, author of the consumer guide to colored gemstones

    琥珀就好比時間膠囊，將某個年代給封鎖住。所以，古生物學家得以重建地球上最原始階段時
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