1)Doushantuoian陡山沱期
1.Megascopic Biota from the Doushantuoian of the Neoproterozoic (Ediacaran) in Guizhou and Zhongqing, South China黔—渝地区新元古代伊迪卡拉纪陡山沱期宏体生物群
2.Emergence of marco-organismal ecosystem of the Late Doushantuoian in South China and its significance华南陡山沱期晚期宏体生物生态系统的出现及其意义
英文短句/例句
1.Emergence of marco-organismal ecosystem of the Late Doushantuoian in South China and its significance华南陡山沱期晚期宏体生物生态系统的出现及其意义
2.Megascopic Biota from the Doushantuoian of the Neoproterozoic (Ediacaran) in Guizhou and Zhongqing, South China黔—渝地区新元古代伊迪卡拉纪陡山沱期宏体生物群
3.New data of phosphatized globular fossils from Weng'an biota in the Ediacaran Doushantuo Formation and the problem concerning their affinity埃迪卡拉纪陡山沱期瓮安生物群中磷酸盐化球状化石新材料及其问题讨论
4.Rock Magnetism of the Carbonates in Doushantuo Formation in Yichang, South China;宜昌陡山沱组碳酸盐岩岩石磁学研究
5.Analyses on the Phosphor-bearing Character of Doushantuo Formation in Machang Area,Guiyang贵阳马场地区陡山沱组含磷特征分析
6.The Microfacies of the Cap Carbonate from the Sinian Doushantuo Formation at the Jiulongwan Section, Yichang, Hubei湖北宜昌九龙湾剖面震旦系陡山沱组盖帽碳酸盐岩微相研究
7.Preliminary Discussion on Phosphorus Seismites from the Ediacaran(Sinian) Doushantuo Formation in South China,and Its Relationship with Meta-biotas华南震旦系陡山沱组磷质震积岩及其与多细胞生物群相关性初探
8.New Advances in the Study of Biostratigraphy of the Sinian(Ediacaran) Doushantuo Formation in South China华南埃迪卡拉(震旦)系陡山沱组生物地层学研究的新进展
9.New Data of Phosphatized Microfossils from the Doushantuo Formation in Baizhu,Baokang County,Hubei Province,and Their Stratigraphic Implications湖北保康白竹陡山沱组磷酸盐化微化石新资料及其地层意义
10.Barite from the Top Ediacaran Doushantuo Formation in the East Yangtze Gorges Area and Its Geological Implications峡东伊迪卡拉纪陡山沱组顶部重晶石特征与地质意义研究
11.Biomarkers of the phosphorites and their indicators of the sedimentary environments of the Doushantuo Formation in Weng'an,Guizhou贵州瓮安陡山沱组磷块岩生物标志物特征及对沉积环境的指示
12.ACRITARCH BIOSTRATIGRAPHIC SUCCESSION OF THE EDIACARAN DOUSHANTUO FORMATION IN THE YANGTZE GORGES峡东地区埃迪卡拉系陡山沱组疑源类生物地层序列
13.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。
14.Rock Magnetism of Greigite-bearing Carbonate Concretions in the upper Doushantuo Formation (South China) and Its Environmental Implications华南陡山沱组四段含胶黄铁矿碳酸盐结核岩石磁学研究及其环境意义
15.Research Advances and Correlations of Carbon Isotopic Compositions in the Ediacaran Doushantuo Formation,East Yangtze Gorges,South China峡东地区埃迪卡拉系陡山沱组碳同位素特征研究进展与国内外对比
16.The airplane zoomed over the top of the mountain.飞机陡直上升，越过山顶。
17.This hill is too steep, your car won't go up这山太陡，你的车上不去。
18.toil up a steep hill吃力地爬一座陡峭的山
相关短句/例句
Late Doushantuoian陡山沱晚期
1.Preliminary discussion on ecological characteristics and buried environments of Miaohe-type Biota during the Late Doushantuoian of Sinian in northeastern Guizhou Province;黔东北震旦纪陡山沱晚期庙河型生物群的生态特征及埋藏环境初探
3)Doushantuo formation陡山沱组
1.Macroscopic Algae from the Ediacaran Doushantuo Formation in Northeast Guizhou, South China;黔东北伊迪卡拉纪陡山沱组的宏体藻类
2.Geochemistry and petrogenesis of the cap dolostones at the bottom of the Doushantuo Formation in northwestern Fanjing Mountains,Guizhou;贵州梵净山西北陡山沱组底部白云岩帽地球化学特征及成因探讨
3.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
4)Doushantuo Formation phosphate rocks陡山沱组磷块岩
1.Plenty of multicellular alage, sponge and embryos have been discovered in the upper Sinian system Doushantuo Formation phosphate rocks(580 million years) in Weng’an county, Guizhou Province.在贵州省瓮安县上震旦统陡山沱组磷块岩（距今５８０ Ｍａ）中，发现有大量的多细胞藻类、海绵和动物胚胎化石。
5)Doushantuo Formation Dengying Formation boundary layer陡山沱组-灯影组界线层
1.Abundant microspherulites have been recently discovered first in the Doushantuo Formation Dengying Formation boundary layer of the Miaohe Sinian section in Zigui, Hubei.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。
6)Doushantuo formation Dengying formation boundary陡山沱组灯影组界线
1.The Doushantuo formation Dengying formation boundary section at Miaohe in the eastern Yangtze Gorges in China is studied.我们研究了峡东庙河陡山沱组灯影组界线剖面，获得ＲＥＥ及其它微量元素异常和大量微球粒等灾变事件的证据，从而判定庙河生物群的大绝灭是由于陡山沱期末的一次地球灾变事件的结果。
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