miocene epoch中文是什么意思
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用"miocene epoch"造句"miocene epoch"怎么读"miocene epoch" in a sentence
中文翻译手机版
- 中新世
- "miocene"中文翻译 n.,adj. 【地质学;地理学】第三纪中新统(的),第 ...
- "epoch"中文翻译 n. 1.纪元,时代;时期。 2.值得纪念的事件[日期] ...
- "miocene" 中文翻译 : n.,adj. 【地质学;地理学】第三纪中新统(的),第三纪中新世(的)。
- "epoch" 中文翻译 : n. 1.纪元,时代;时期。 2.值得纪念的事件[日期]。 3.【地质学;地理学】世,纪,期。 4.【物理学】初相;【天文学】历元;【电学】(信号)出现时间,恒定相位延迟。 mark [form] an epoch (in)… (在…上)开辟新纪元。
- "eocene-miocene" 中文翻译 : 始新-中新世
- "mintzberg miocene" 中文翻译 : 中新世的
- "miocene clay" 中文翻译 : 中新世粘土
- "miocene period" 中文翻译 : 中新世
- "miocene series" 中文翻译 : 中新统
- "pre-miocene" 中文翻译 : 中新世前的
- "shanwang miocene flora" 中文翻译 : 山旺中新世植物区系,山旺中新世植物群; 山旺中新世植物群
- "alluvial epoch" 中文翻译 : 冲积期; 冲积世
- "baseleveling epoch" 中文翻译 : 均夷期
- "baselevelling epoch" 中文翻译 : 均夷期
- "cambrian epoch" 中文翻译 : 寒武世
- "decoupling epoch" 中文翻译 : 退耦期
- "degrading epoch" 中文翻译 : 夷低期
- "diluvial epoch" 中文翻译 : 【地质学;地理学】洪积世。
- "drift epoch" 中文翻译 : 流冰期
- "dry epoch" 中文翻译 : 干燥期
- "eocene epoch" 中文翻译 : 【地质学;地理学】始新世。
- "epiglacial epoch" 中文翻译 : 冰缘期
- "epoch angle" 中文翻译 : 初相角
- "epoch hotel" 中文翻译 : 天新饭店
- "epoch making" 中文翻译 : 划时代的
例句与用法
- Therefore , the thesis thinks wudaoliang group and suonahu formation are the outcome of the miocene epoch
因此,论文认为五道梁群和唢呐湖组都是中新世时期的产物。 - They are all called yangping period denudation surface and were formed in the miocene epoch and the pliocene epoch
鲁中南山地东部山顶部位的熔岩被分布面也相当于仰平期剥夷面。 - Synthesizely contrasted the suonahu formation profile of the northern qiangtang basin and cuoqin basin of miocene epoch , used the intraclast ash rock as the marker bed of the suonahu formation
对羌北盆地和措勤盆地中新世的唢呐湖组剖面作了综合对比,将内碎屑灰岩作为唢呐湖组的标志层。 - Finally , author have discussed the relationship transformation process of the honghe fault shear mode and block movement , proofed that the eta - type tectonic system was formed in miocene epoch
讨论了红河断裂剪切方式的转变过程与岩块运动的关系,论证了歹字形构造体系形成于约20ma的中新世时期。 - The thesis analysises the typical model profile and the special rock profile of wudaoliang group of miocene epoch in hoh xil basin . and be used the biocalcarenite with the marl rock take the marker bed of wudaoliang group
论文对可可西里盆地中新世五道梁群的典型剖面和特殊岩性剖面进行了分析,并以泥灰岩和生物碎屑灰岩作为五道梁群的标志层。 - Comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period , expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch , warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
通过对云南景谷盆地及陇川盆地新生代生物群特征的对比,探讨了新生代两大盆地环境演变:早中新世到上新世为湖盆发展期湖盆扩大萎缩期,气候为早期的千燥中新世早期的温暖湿润中新世中晚期的寒冷阴湿上新世的干燥,而中新世中晚期湖盆的扩大形成的半深湖深湖环境为油气的形成提供了有利条件。 - Abstract : comparison and study of the biotic characters in the jinggu and longchuan basins in yunnan province show that : ( 1 ) the two basins underwent the developing period , expanding period and shrinking period from early miocene epoch to pliocene epoch ; ( 2 ) the climate in the region was dry in early miocene epoch , warm and humid in middle - late miocene epoch and dry in pliocene period ; ( 3 ) the basins expanding in middle - late miocene epoch formed a semi - deep - lake to deep - lake environment
文摘:通过对云南景谷盆地及陇川盆地新生代生物群特征的对比,探讨了新生代两大盆地环境演变:早中新世到上新世为湖盆发展期湖盆扩大萎缩期,气候为早期的千燥中新世早期的温暖湿润中新世中晚期的寒冷阴湿上新世的干燥,而中新世中晚期湖盆的扩大形成的半深湖深湖环境为油气的形成提供了有利条件。 - The volcanic rock age and the age of the qiangtang formation determined the wudaoliang group between 20 - 5ma , discovering a flood of spore and pollen with ostracods fossils ( regard eucypris as principle ) , which are miocene epoches typical numerator , therefore wudaoliang group accumulate in miocene epoch is doubtless ; 9 - 2ma are the age of the suonahu formation based on the data of the esr , which were characteristic of later period in miocene epoch - pliocene epoch , spore and pollen with fossil all were miocene epoch period
由火山岩和覆于其上的羌塘组的年龄限定五道梁群的沉积时间为20 - 5ma ,五道梁群中发现大量的孢粉和介形虫化石(以eucypris为主) ,分析认为它们都是中新世时期的典型分子,因此五道梁群的沉积时间为中新世是无疑的;唢呐湖组的esr测年数据范围为9 - 2ma ,代表中新世晚期?上新世时期,孢粉和化石都具有中新世时期的特征。
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