震旦系的英文

音标：[ zhèndànxi ] 发音:

"震旦系"怎么读用"震旦系"造句

英文翻译手机版

sinia ystem
sinian system

"系"英文翻译 system; series
"震旦纪；震旦系" 英文翻译 : sinian
"震旦" 英文翻译 : zan tahn
"震旦报" 英文翻译 : aurore l'; l' aurore
"震旦龟" 英文翻译 : sinochelys
"震旦纪" 英文翻译 : ediacaran; sinian period
"震旦龙" 英文翻译 : sinosaurus
"前震旦纪" 英文翻译 : pre-sinian
"上震旦统" 英文翻译 : upper sinian series
"晚震旦世" 英文翻译 : late sinian epoch
"早期震旦纪" 英文翻译 : kaolan(series
"震旦半椎鱼" 英文翻译 : sinosemionotus
"震旦笔石" 英文翻译 : sinograptus
"震旦大学" 英文翻译 : aurora university
"震旦方向" 英文翻译 : sinian trend; siniantrend
"震旦复兴" 英文翻译 : the revival of china -- return of prosperity
"震旦海百合" 英文翻译 : sinocrinus
"震旦海林擒" 英文翻译 : sinocystis
"震旦河南" 英文翻译 : sinohadvianus
"震旦角石" 英文翻译 : sinoceras
"震旦珊瑚" 英文翻译 : sinophyllum
"震旦石燕" 英文翻译 : sinospirifer
"震旦索氏虫" 英文翻译 : sinosaukia
"震旦鸦雀" 英文翻译 : reed parrotbill; yangtze crowtit
"震旦原始介" 英文翻译 : sinoprimitia

例句与用法

The sedimentary environment of grapestone in dengying formation of sinian system in sichuan nad yunnan
川滇震旦系灯影组葡萄石的沉积环境
Sedimentary successions and environment of the sinian doushantuo formation in jiangkou , guizhou province
贵州江口震旦系陡山沱组沉积层序和沉积环境分析
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:在湖北秭归庙河震旦系剖面陡山沱组-灯影组界线层内首次发现了微球粒。
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
摘要广东广宁厚溪铌钽矿床赋存于震旦系c组地层中，区内褶皱构造、断裂构造十分发育。
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
新方案中这些地层在我国晚前寒武纪地层柱中的位置，反应出了震旦系与青白口系的地史演化及生物演化间的重要关系。
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
摘要阿牙登组和腮林忽洞组是上世纪70年代1 / 20万区调建立的地层单位，当时将阿牙登组置于白云鄂博群，腮林忽洞组归于震旦系。
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
本文依据地层接触关系的类型和规模，将本区划分为基岩(前震旦系) 、下(古生界) 、中(中生界) 、上(新生界)四个构造层和内部的七个构造亚层。
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
通过对黄连坑锰矿区地层的含矿性、控矿构造及容矿构造、矿体特征、矿石类型等地质特征的论述，认为震旦系地层是“初始矿源层” ，滑脱构造对成矿物质起迁移、富集及容矿作用。
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
摘要本文通过对相山火山盆地基底震旦系浅变质岩、盖层火山岩稀土元素分布特徵的研究，探讨相山火山岩的物质来源及岩石成因，认为相山火山岩主要是上部地壳重熔的产物，其岩石成因应属于重熔型花岗岩的?畴。
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
矿床地质特征以及常微量元素、稀土元素、同位素、成矿流体等地球化学特征的研究表明，矿床成矿物质是多来源的，天宝山矿床成矿物质主要来自上部地壳和造山带各种沉积岩，大梁子矿床成矿物质主要来自震旦系灯影组地层；两个矿床成矿溶液主要来自大气降水；硫大部分来源于同时期的海相沉积地层(震旦系灯影组)中被细菌还原的海水硫酸盐。