秦南 的英文怎麼說

中文拼音 [qínnán]
秦南 英文
qinnan
  • 秦 : 名詞1 （周朝國名） qin a state in the zhou dynasty2 （朝代） the qin dynasty （221 206 b c ）3 （...
  1. Webzine and poetry resource offering original poems, essays, translations and links to alliterative poems, original medieval epics and verse romances

    -中國詩歌研究，研究著作，研究學者，詩歌常識及自先秦漢魏晉南北朝的古代詩歌。
  2. From the middle devonian to the early carboniferous, the spores of the shishuyuan trough in the northern part of eqm and those of the nanwan trough in the southern part of eqm belonged to the south china province, and the late devonian corals, brachiopods, plants, and the early carboniferous fusulinids of the xichuan shelf were from the south china province

    在中泥盆世至早石炭世，東秦嶺北部柿樹園海槽與東秦嶺南部南灣海槽的孢子及浙川陸棚的晚泥盆世珊瑚、腕足類和古植物及早石炭世（蟲? ）屬華南生物省。
  3. From the cambrian to the early middle ordovician, the cambrian radiolaria and the early ordovician conodonts of the erlangping trough in the northern part of eqm, and the cambrian trilobites and early ordovician conodonts as well as cephalopods of the northern xichuan shelf in the southern part of eqm belonged to the south china province, while the cambrian trilobites and the early ordovician conodonts of the southern xichuan shelf belonged to the south china province with some elements of the north china province

    在寒武紀至中奧陶世早期，東秦嶺北部二郎坪海槽的寒武紀放射蟲和早奧陶世牙形石與東秦嶺南部浙川陸棚北部的寒武紀三葉蟲、早奧陶世牙形石和頭足類屬華南生物省，而浙川陸棚南部的寒武紀三葉蟲和早奧陶世牙形石屬于華南生物省，兼有華北生物省分子。
  4. Qinling fold belt is located at the junction of the north china plate and the yangtze plate, and its portion in henan province is a part of the east qinling mountains ( eqm )

    摘要秦嶺褶皺帶位於華北板塊和揚子板塊結合部位，其在河南省內的部分多劃為東秦嶺。
  5. Country seat of licheng in qin and han dynasty, double city in wei and jin southeast dynasty, mother - son city of qi and state

    濟南古城，經歷了歷下古城堡、秦漢歷城縣城、魏晉南北朝「雙子城」 、齊州州城（母子城）和濟南府城的演變過程。
  6. Artists : anothermountainman, terry batt, david boyce, bowles chan, joe chan, chris chan kam - shing, dick chan kwongyuen, chan muk - nam, raymond chan waiman, teresa chan wai - sze, enoch cheung hong - sang, cheung king - ling, cheng yat - yue, chun wai, david clarke, jayne dyer, livia b. garcia, alex heung kin - fung, monti lai wai - yi, carol lee mei - kuen, ceci liu wai - yee, cheung wai - lok, mak siu - fung, stanley ng waicheong, fran van riemsdyk, jose manuel sevilla, jacky sin, so hing - keung, leon suen shu - kwan, lukas tam wai - ping, tang ying - chi, tang ying - mui, oliver tsang, ducky tse, tse ho - yin, tse ming - chong, kevin white, edmond wong, kacey wong, wong kan - tai, bobby yip, yip kin - yiu, vincent yu the coming july is the decennial of hong kongs return to china, too art and lumenvisum have prepared a gift to everybody

    藝術家又一山人、泰利百特、 david boyce 、陳錦輝、陳貴明、陳錦成、陳廣源、陳木南、陳偉民、陳慧思、張康生、張景寧、鄭逸宇、秦偉、祈大衛、 jayne dyer 、陳令芯、香建峰、黎慧儀、李美娟、廖慧怡、張偉樂、麥兆豐、伍偉昌、 fran van riemsdyk 、 jose manuel sevilla 、單麒澤、蘇慶強、孫樹坤、譚偉平、鄧凝姿、鄧凝梅、曾維德、謝至德、謝浩然、謝明莊、白啟仁、黃文山、黃國才、黃勤帶、葉英傑、葉堅耀、余偉建
  7. The controlling parameters for smooth blasting in qin - ling zhongnanshan tunnel project are optimized according to the fundamental principle of smooth blasting, considering the minimal resistance, coefficient of embrasure density, coefficient of non - coupling, density of dynamite and rate of exploding. the efficiency of this method has been analyzed and justified by the high speed and good quality of the project

    根據光面爆破的基本原理，從最小抵抗線、爆眼密集系數、不耦合系數、線裝藥密度、爆破進尺等幾個方面確定秦嶺終南山隧道光面爆破主要參數的選取，分析了該隧道鉆爆設計在隧道施工中的運用取得的成效，提高了施工進度，同時也保證了施工質量。
  8. The faunal study on the butterflies of the south slope of qinling mountains

    秦嶺南坡蝶類區系研究
  9. Based on the analysis of the data on global metallogeny in the framework of geodynamics and study of the processes of continental evolution and metalloeny of of sanjiang, qinling and xingan - mongolia orogenic belts, we have reconsidered the geodynamic evlution and metallogeny during indosinian to early - yanshan movement in china, and established large - scale metallogenic model on intracontinental evolution we in orogenic belts. the main results are summarized as follow. ( 1 ) systematically gathering the data about large - scale and superlarge - scale deposits in the world and drawing up the map of global tectonics and metallogeny ; finding out the segmentation of circle - pacific ocean metallogenic belt and informing that the giant deposit clusters are the prominent feature of global metallogeny

    本文在總結全球大規模成礦的地球動力學背景資料基礎上，通過深入解剖和系統對比我國三江造山帶南段、東秦嶺造山帶和興蒙造山帶中南部等典型造山帶關鍵地區以陸內演化過程為核心的地球動力學演化歷史及其成礦特徵，重新認識了我國大陸印支?早燕山期的動力學演化過程及其成礦效應，建立了關于造山帶陸內演化階段主要過程中的大規模成礦模式。
  10. The fossils of three species : microtus oeconomus, caryomys eva and c. inez from luonan zhangping, shaanxi province are studied in this paper

    秦嶺是中國南北地理、氣候和生物的分界線，對中國南北的氣候環境具有重要的屏障和分異作用。
  11. Conclusion the taihua complex in the area is a metamorphic complex undergone low - angle overthrust from the south to the north and uplifting lately by fault blocking, rather than a mcc

    結論小秦嶺地區的太華雜巖解釋為經歷了從南向北的鏟狀逆沖推覆和後期抬升塊斷剝露的變質雜巖更為合理。
  12. The number of species in the southern slope of qinling mountain was most abundant because of distribution of some palaearctic species to the top of qinling mountain, especially species of oedipodidae, another reason may b. e the large number of endemic species in this area

    秦嶺南坡種類最多，主要是有部分古北界的種類滲透分佈在中、高山地帶，特別是斑翅蝗科的種類，另外還有部分特有種。
  13. General ching's resolute group moved south from honan province.

    秦將軍帶領的這支患難與共的隊伍從河南府往南移動。
  14. The vegetation type was classified in the east transect by unsupervised classification using the data ( ikmx 1km ) from noaa meteorology satellite from 1995 - 1996, and the article analyzed the change of ndvi of all kinds of vegetation types, in the same time analyzed the forest dynamics in typical ecotone ( warm temperate zone to semitropical in qinling woods ) using the higher spatial resolution tm data

    本論文利用1995 - 1996年noaa氣象衛星的ndvi （ 1km 1km ）數據，採用無監督分類方法對中國東部樣帶南方部分進行植被類型的劃分，分析各植被類型的ndvi變化情況；並利用較高精度的tm數據分析典型交錯區域（暖溫帶到亞熱帶的秦嶺林區）的森林動態變化情況。
  15. Based on the two ctd data sets from the cruise of the summertime in 2000 and wintertime in 2001 in bohai sea and the collected historic observed thermohaline data, we analyse systemically the distributional characteristics of temperature, salinity and density in wintertime and summertime in the bohai sea and the results reveal that the current hydrologic characteristics of the bohai sea have some obvious variances relative to the previous research results. in summer there are three low - temperature centers in the middle - layer and underlayer of the middle parts of the bohai strait, liaodong bay - mouth and bohai bay - mouth, but there is a uniform high - temperature center in the middle part of the bohai sea. in winter the isotherms extend westward and northward to the bohai sea from the warm core of the bohai strait and a cold - water tongue off the qinhuangdao spreads southeastward out, so the saddle - like isotherm pattern is formed in the middle part of the bohai sea

    利用2000年夏季和2001年冬季渤海兩次ctd資料和以前收集的渤海溫鹽調查資料，分析了渤海冬、夏季溫鹽密度的分佈特徵，結果表明，渤海現有的水文特徵與以往研究結果相比發生了明顯的變異：夏季在渤海海峽、遼東灣口和渤海灣口中部中、下層存在三個低溫中心，在渤海中部則出現一個上下均勻一致的高溫中心；冬季等溫線以渤海海峽暖中心向西和向北兩個方向伸入渤海，而從秦皇島外海有一冷水舌向東南方向伸展，在渤海中部海域形成「馬鞍狀」等溫線結構。
  16. On the basis of the types of sand stone, light and heavy mineral associations, planimetric map of sedimentary facies and directions of palaeoflow, it is considered that detrital material of terrigenous deposit of chang6 - 8 oil - beds in this area come from southwest provenance, northeast provenance, west provenance and south provenance, respectively, which are the denudation area of huating - longxian county in southwestern, yinshan ancient land in the northern, the denudation area of yantong mountain and tongxin to the west of yangjiajuzi - yinjiacheng county and qinling ancient land in the southern

    根據砂巖類型、輕、重礦物組合、沉積相帶平面展布及古水流方向等特徵的分析，認為研究區延長組長6 ? 8油層組陸源碎屑物質來自西南、東北、西部和南部四大物源區，分別為西南華亭?隴縣一帶剝蝕區，北部陰山古陸，西部的楊家咀子、殷家城以西的煙筒山、同心地區剝蝕區和南部秦嶺古陸。
  17. From february to august 2000, nayang municipal institute of cultural relics and archaeology excavated two burials of the qin dynasty at the site of nanyang municipal office for housing removing program, yielding several bronze vessels of the qin dy nasty and providing valuable materials for studying burial customs and other aspects of the qin culture

    2000年2月- 8月，南陽市文物考古研究所為配合基本建設在南陽市拆遷辦工地發掘秦基2座，出土秦代銅器數件，為南陽地區秦代埋葬風俗及秦文化的研究提供了寶貴的實物資料。
  18. It could be evident that the age of cave fauna is the mid - late pleistocene, according to the three fossil species comparing with those of other fossil faunas related sites and according to the river terraces analysis near by luohe river

    「陜西洛南張坪田鼠類化石研究」就是這項工作的一小部分，目的是為認識秦嶺的隆升及環境變遷提供更多的證據。
  19. The spot coal price decline would benefit huaneng the most, as it ( i ) buys 35 % of its coal from spot market ( versus 10 % for its peers ) and ( ii ) has 10, 777mw ( 38 % ) attributable capacity ( the most among them ) in coastal southeast provinces with coal supply via qinhuangdao

    煤炭價格的下跌中，華能受益最大，這是因為1 ）它有35 %的煤炭從市場上購買（而同行僅需10 % ） ， 2 ）通過秦皇島的煤炭供給向南部沿海各省輸送1077 . 7萬千瓦（ 38 % ）的電能。
  20. 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。
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