震旦紀 的英文怎麼說

中文拼音 [zhèndànjì]
震旦紀 英文
ediacaran
  • 震 : Ⅰ動詞1 （震動） quake; shake; shock; vibrate 2 （情緒過分激動） be greatly excited; be deeply ast...
  • 旦 : 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...
  • 紀 : 紀名詞（姓氏） a surname
  • 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震旦紀基底地層為：晚太古代-新元古代米蘭巖群，長城系卡羌巖群，薊縣系流水巖組和青白口系絲路巖組。
  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. The main diagenetic stage and relevant rock types are the middle proterozoic assemblage of gneissoid granodiorite - adamellite and the sinean schistosity diorates

    主要成巖期及代表性巖類有：中元古界為片麻狀花崗閃長巖二長花崗巖，震旦紀為片理化閃長巖。
  4. 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系統在防盜方面有獨到之處，一旦盜竊者有撬門或破壞鎖具，門鎖的鎖栓震動，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。
  5. The reefs widely developed from sinian to neogene in china, with main reef - forming stages in devonian, permian and neogene, respectively

    摘要中國生物礁從震旦紀至新近紀均有發育，分佈范圍廣，並有泥盆紀、二疊紀和新近紀3個主要造礁期。
  6. We have concluded that the structural movement of the area can be divided into three stages : the stretching stage from simian to early ordovician, the extrusion and rising stage from middle and late ordovician to jurassic and stable depressed stage of foreland basin slope from cretaceous to neozoic

    經研究認為研究區的構造運動，主要分為震旦紀到早奧陶世的拉張階段、中晚奧陶世到侏羅紀的擠壓隆升剝蝕階段以及白堊紀到新生代的前陸盆地斜坡穩定沉降階段。
  7. 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層可劃分為五大構造層序，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、中新元古代克拉通內裂陷槽或坳拉槽演化階段、震旦紀?早古生代華北陸表海盆演化階段、晚古生代?早中生代華北克拉通坳陷演化階段、中生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、新生代周緣斷陷盆地演化階段。
  8. In a study on a sedimentary basin analysis of the huanan orogenic belt, the sedimentary basin character and evolution in the southeastern passive continental margin of the yangtze plate is investigated with elaborate sedimentary environments and sedimentary character from the sinian to the triassic, and then the sedimentation sketch of this belt is established especially to be from rift, passive continental margin into foreland basin in the early paleozoic on the yangtze plate

    在華南造山帶沉積盆地分析和演化研究中，對揚子大陸東南邊緣從震旦紀到三疊紀沉積環境，沉積作用特點，沉積盆地性質和演化進行研究，特別是建立了中國南方揚子板塊早古生代從裂谷，被動大陸邊緣到前陸盆地華南造山帶沉積作用格架。
  9. Sedimentation - diagenesis deposits mainly formed during late sinian to cambrian period, such as bingtongshan pbzn deposits and aozigang deposits

    沉積成巖型鉛鋅礦主要成礦時代屬晚震旦世~寒武紀，如冰洞山式鉛鋅礦床和凹子崗鋅礦床。
  10. The sinian granitoids are immediately related the plate collision, they were formed in the plate collision mounain - building period - post collision elevation period

    震旦紀花崗巖類與板塊碰撞作用密切有關，是碰撞造山一碰撞后抬升這一過程形成的花崗巖類。
  11. New observations on phosphatized spheroidal fossils in sinian doushantuoan phosphorites in weng an, guizhou province

    貴州甕安震旦紀陡山沱期磷酸鹽化球狀化石的新觀察
  12. 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 、盆地自震旦紀以來長期接受沉積，地層發育良好，震旦紀至中三疊世為海相沉積體系，晚三疊世以後為陸相沉積體系。
  13. Geological characteristics of the metamorphic conglomerate in sinian stratigraphy in the luoding area, the western guangdong

    羅定地區震旦紀地層中變質礫巖的地質特徵
  14. During the sinian, a series of catastrophic events occurred in the eastern part of the yangtze gorge, including hot, cold and gravity events

    摘要長江三峽東部地區震旦紀先後發生了熱事件、冷事件、重力事件等突發性災變沉積。
  15. The minerogenetic epoch lasted from paleoarchean to sinian, with neoarchean, paleoproterozoic and mesoproterozoic - qingbaikouan being the culmination periods

    成礦時代從古太古代到震旦紀，但以新太古代、古元古代、中元古代青白口紀3個地質時期為成礦高峰期。
  16. 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系，同時斷裂活動表現為多期性和繼承性的特點；該區經歷了震旦紀至早奧陶世、早奧陶世末志留紀、侏羅系、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。
  17. 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；處於前震旦紀變質巖系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。
  18. 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系的地史演化及生物演化間的重要關系。
  19. 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。
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