震旦 的英文怎麼說
中文拼音 [zhèndàn]
震旦
英文
zan tahn-
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。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。Cold event deposits were developed in the nantuo formation of the lower sinian and should be continental glacial deposits in a low - latitude and low - altitude area
冷事件沉積產物為下震旦統南沱冰磧層，屬低緯度低高程的大陸冰川沉積。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。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。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。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。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。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。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
本商行經營震旦、榮仕寶、萬能通、財利隆、快靈通、卡邁仕等系列中、高檔國產計算器、卡西歐、佳能、夏普等系列進口計算器、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。In the early sinian, clastic sediments formed by fluvial and continental glacial actions were developed, while in the late sinian, great thickness of marine carbonate rocks formed by two transgression - regression cycles were developed
早震旦世發育由河流作用與陸地冰川作用形成的陸源碎屑沉積；晚震旦世則發育由兩次臺地盆地臺地的海進海退旋迴形成的巨厚海相碳酸鹽沉積。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系的類型和規模，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。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。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Hot event deposits occurred in liantuo formation of lower sinian, interbedded in fluvial facies sandstones and siltstones
熱事件沉積產物見于下震旦統蓮沱組，夾于河流相沉積的砂巖及粉砂巖中。The gravity events include slumping event and turbidity - current event, and the gravity event deposits were developed in deep - water carbonate rocks in the upper sinian
重力事件可分為滑塌事件和濁流事件，其沉積產物均分佈於上震旦統，夾在大套的深水碳酸鹽巖中。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。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。分享友人