震旦系 的英文怎麼說

中文拼音 [zhèndàn]
震旦系 英文
sinia ystem
  • : Ⅰ動詞1 (震動) quake; shake; shock; vibrate 2 (情緒過分激動) be greatly excited; be deeply ast...
  • : Ⅰ名詞1 [書面語] (天亮) dawn; daybreak 2 (天) day 3 (戲曲中扮演婦女的角色) the female charac...
  • : 系動詞(打結; 扣) tie; fasten; do up; button up
  • 震旦 : zan tahn
  1. It agrees with the fact that the gabbro is intruded by late ordovician granitic pluton. the pre - sinian basement strata exposed in the north kunlun massif are later archean - neoproterozoic milan group, changcheng system kaqiang group, jixian system liushui formation and qingbaikou system sulu formation

    被蛇綠巖所分隔的昆北地塊上出露的前紀基底地層為:晚太古代-新元古代米蘭巖群,長城卡羌巖群,薊縣流水巖組和青白口絲路巖組。
  2. The sedimentary environment of grapestone in dengying formation of sinian system in sichuan nad yunnan

    川滇震旦系燈影組葡萄石的沉積環境
  3. The systems of century ck security locks and automatic alarm lock security have special features, when the larcener were seen breaking a lock, the setbar of door lock shock, it automatically switches touch alarm, it quickly issued a warning signal, alarm and transmitted to the mainframe, telecommunications company by phone or sent to the terminal, it can be 110 and the security alarm centers, community policing, the residential quarters network security departments, the police realized the linkage

    世紀西科防盜鎖具及自動報警防盜鎖具統在防盜方面有獨到之處,一盜竊者有撬門或破壞鎖具,門鎖的鎖栓動,能自動觸動報警開關,迅速的發出報警信號,並傳送到報警主機上,通過電信公司發送至手機或電話終端;可以與公安110報警中心,社區治安聯防,住宅小區保安部門聯網,實現了聯動報警。
  4. The firm deals in aurora, rsb, w. n. t, caielon, k. l. t, castalent, etc. high & middle - grade national calculators, and casio, canon, sharp, etc imported calculators, as well as office appliances such as various cash counters, electronic notebooks, paper shredders, etc

    本商行經營、榮仕寶、萬能通、財利隆、快靈通、卡邁仕等列中、高檔國產計算器、卡西歐、佳能、夏普等列進口計算器、各種點鈔機、電子記事本、碎紙機等辦公用品,同時可代客加工特製各種計算器。
  5. According to the type and scale of stratigraphic contact, four synthems such as basement ( pre - sinian ), lower ( palaeozoic ), middle ( mesozoic ) and upper ( cenozoic ) are divided, and seven sub - synthems are subdivided

    本文依據地層接觸關的類型和規模,將本區劃分為基巖(前震旦系) 、下(古生界) 、中(中生界) 、上(新生界)四個構造層和內部的七個構造亞層。
  6. Sedimentary successions and environment of the sinian doushantuo formation in jiangkou, guizhou province

    貴州江口震旦系陡山沱組沉積層序和沉積環境分析
  7. Conclusion are obtained as follows : 1. basin accepted sedimentation since sinian, and strata were well developed. it was marine sedimentary series from sinian to middle - triassic and become continental sedimentary series since late - triassic

    主要成果及認識如下: 1 、盆地自紀以來長期接受沉積,地層發育良好,紀至中三疊世為海相沉積體,晚三疊世以後為陸相沉積體
  8. Abstract : abundant micrcspherulites have been recently discovered first in the doushantuo formation - dengying formation boundary layer of the miaohe sinian section in zigui, hubei

    文摘:在湖北秭歸廟河震旦系剖面陡山沱組-燈影組界線層內首次發現了微球粒。
  9. Haoxi nb - ta mineral deposits in guangning county of guangdong province occurs in the c - formation of sinian system strata and the folding structures and faulted structures is a very development in the area

    摘要廣東廣寧厚溪鈮鉭礦床賦存於震旦系c組地層中,區內褶皺構造、斷裂構造十分發育。
  10. Multistage structural deformations are experienced in kongquehe area, the basical fault systems of nww - near ew, nne - near sn, nnw and nee are established, the fault movement has the characteristics of multistage and inheritance, in the area multi - structural deformations are experienced in sinian to early ordovician, early ordovician - silurian, jurassic cretaceous - caenozoic, etc. late structural deformation shapes are changed for different levels of formar structural layer, in which different deforming shapes are created and integrated overlying of deformation is induced

    摘要孔雀河地區經歷了多期次的構造變形作用,形成了現今北西西近東西向、北北東近南北向、北北西向和北東東向基本斷裂體,同時斷裂活動表現為多期性和繼承性的特點;該區經歷了紀至早奧陶世、早奧陶世末志留紀、侏羅、白堊紀新生代等多期構造變形作用,且後期的構造變形作用在不同程度上對前期的構造層的變形樣式有所改造,形成了有一定差異的變形面貌,造成變形的復合登加。
  11. Studies on geology of the deposits and geochemistry of trace elements, rees, isotopes, ore - forming fluids show that the ore - forming materials came from varied sources. ore - forming materials of the tianbaoshan deposit was chiefly derived from different sedimentary rocks of the upper crust and orogen, while those of the daliangzi deposit mainly from the sinian dengying formation. meteoric waters were the major source of the ore - forming solution

    礦床地質特徵以及常微量元素、稀土元素、同位素、成礦流體等地球化學特徵的研究表明,礦床成礦物質是多來源的,天寶山礦床成礦物質主要來自上部地殼和造山帶各種沉積巖,大樑子礦床成礦物質主要來自震旦系燈影組地層;兩個礦床成礦溶液主要來自大氣降水;硫大部分來源於同時期的海相沉積地層(震旦系燈影組)中被細菌還原的海水硫酸鹽。
  12. The lower paleozoic continent marginal sedimentary strata in the north kunlun massif are sinian - cambrian alajiaoyi group and ordovician pishigaisayi formation. the former is composed of high maturity flysch deposit, the later consist of continental shelf deposit such as carbonate and slate and sandstone. these rocks implies that they might form at passive continental margin

    與其曼于特蛇綠巖相關的早古生代邊緣沉積巖在昆北地塊上為?寒武阿拉叫依巖群、奧陶皮什蓋薩依巖組,前者為一套成熟度較高的陸源碎屑復理石沉積,後者為碳酸鹽巖和含碳板巖砂巖等陸棚沉積,顯示其具被動陸緣性質。
  13. In qinghai province, it reveals that the au deposits are mostly distributed on the sits between different tectonic units ; and in the edge of the exposed and / or concealed metamorphic basement of the early sinian period ; in the area of the exposed and concealed acid - instrusions and / or their contacts ; and in the localities where the circular and linear anomalies of graviation and magnetism cut across

    結果表明,該區的金礦大都分佈在不同大地構造單元結合部位;處於前紀變質巖出露及隱伏基底邊緣;位於出露和隱伏中酸性巖體及其接觸帶;位於重磁環線、線線構造交匯處等。
  14. In 1917 he went to japan to learn painting. in 1918 he became an adviser in the painting research institute of beijing university

    1916年入上海圖書美術館及上海大學法文半工半讀, 1917年赴日本學習美術, 1918年在北京大學畫法研究會擔任導師。
  15. During the work period in the southern zone of the east qinling belt, the process of sedimentation, basin quality and its interior structure and configure, important events are studied from the sinian to the triassic, especially through more than one hundred km profile across the southern zone of the east qinling belt. in the technical method, the basin dynamic analysis in the cambrian and the devonian respectively and the cycle events in the late triassic are added to the research of the belt. the some basic and important viewpoints of the orogenic - sedimentology are prompted in the study method, thought and connotation fields in this stage

    在東秦嶺南帶沉積盆地演化研究中:通過對東秦嶺南帶從繫到三疊的沉積作用過程,沉積環境展布和變化,沉積盆地性質、內部結構、層序、配置和發展演化,沉積過程中重大地質事件研究;隨著全球沉積地質計劃在全球的推廣和展開,在研究內容和技術方法上,增加秦嶺造山帶層序地層學以及沉積盆地動力學探索等沉積地質學前緣學科的研究,這樣從更深入和更廣闊的角度進行了這個造山帶的沉積盆地分析,在研究方法、思路和內涵上開拓了造山帶沉積學的一些基本觀點。
  16. Through the analysis of geological characters in huanglianken manganese ore district, such as ore potentiality, ore controlling structures, ore depositing structures, orebody characteristics, ore type and so on, the author concluded that sinian stratum is the " primary source bed ", detachment structure is the migrating channel of ore - forming materials, favorable concentration and hosting place

    通過對黃連坑錳礦區地層的含礦性、控礦構造及容礦構造、礦體特徵、礦石類型等地質特徵的論述,認為震旦系地層是「初始礦源層」 ,滑脫構造對成礦物質起遷移、富集及容礦作用。
  17. In the new plan, the position of the studied strata in the stratigraphic column of late precambrian of china shows an impotant relation between sinian system and qingbaikou system on the geologic and biologic evolution

    新方案中這些地層在我國晚前寒武紀地層柱中的位置,反應出了震旦系與青白口的地史演化及生物演化間的重要關
  18. The ayadeng and sailinhudong formations were established in the 1970 ' s by the regional geological survey, and the former was considered to belong to the proterozoic baiyunebo group and the later belonged to the sinian system

    摘要阿牙登組和腮林忽洞組是上世紀70年代1 / 20萬區調建立的地層單位,當時將阿牙登組置於白雲鄂博群,腮林忽洞組歸于震旦系
  19. Based on the study on ree distribution characteristics of sinian low grade metamorphic rocks of the basement and cover volcanics, the author makes a discussion on the material source and the genesis of xiangshan volcanics, and suggests that xiangshan volcanics came mostly from the remelting of the upper crust, and the genesis should be attributed to the category of remelted granites

    摘要本文通過對相山火山盆地基底震旦系淺變質巖、蓋層火山巖稀土元素分佈特徵的研究,探討相山火山巖的物質來源及巖石成因,認為相山火山巖主要是上部地殼重熔的產物,其巖石成因應屬于重熔型花崗巖的?疇。
  20. The global financial system is facing an unprecedented confluence of risks and, as a very open international financial centre, hong kong may get a disproportionate share of financial market volatility, particularly when some of those risks materialise

    全球金融體正面臨前所未有的風險匯聚情況,一風險演變成蕩,香港這個開放的國際金融中心便可能會面對特別厲害的市場波動。
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