说明:双击或选中下面任意单词,将显示该词的音标、读音、翻译等;选中中文或多个词,将显示翻译。
您的位置:首页 -> 词典 -> 二叠纪-三叠纪牙形石
1)  Permian-Triassic conodont
二叠纪-三叠纪牙形石
2)  Permian-Triassic
二叠-三叠纪
3)  Carboniferous-Triassic
石炭纪-三叠纪
4)  Carboniferous-Permian
石炭-二叠纪
1.
Deformation and metamorphic characteristics of Carboniferous-Permian coal-bearing formation and related geological hazards in Xishan (Western Hills), Beijing;
北京西山石炭-二叠纪煤系变形变质特征与地质灾害
2.
Analysis of Sedimentary Environment and Ascertainment of Carboniferous-Permian Lithostratigraphic Unit in South Area of Beishan, Xinjiang;
新疆北山南部地区石炭-二叠纪岩石地层单位厘定及沉积环境分析
3.
Geochemistry of the Carboniferous-Permian post-collisional granitic rocks from Tianshan;
天山石炭-二叠纪后碰撞花岗质岩石地球化学研究
5)  permo-carboniferous
石炭二叠纪
1.
The Cathaysia flora, which mainly flourished during the Permo-Carboniferous time in East Asia, has been held consistently in geology and palaeontology at home and abroad.
主要繁盛于东亚石炭二叠纪的华夏植物群(Cathaysiaflora)早已驰名中外,且在地质古生物界始终有着一致认识。
2.
n the basis of new viewpoint of stratigraphic correlation and by using highresolution map-making technology, a series of maps about transgressive rangs and directionshave been finished through the detailed study marine beds(limestons and marine mudstons) distributions in Permo-Carboniferous System of North China.
以新的地层对比意见为基础,通过对华北石炭二叠纪海相层(石灰岩和海相泥岩)分布的详细研究,应用高分辨编目技术,完成了石炭二叠纪各期海侵范围及海侵方向图件的编制,并着重指出:①在晚石炭世早期(晋祠期)以前,郯庐断裂以西的海侵方向主体为由东向西,海侵作用中心具有由南向北迁移的规律;②自晚石炭世晚期(太原期)开始,华北盆地构造发生大的变动,古斜坡由北倾变为南倾。
6)  Permo-Carboniferous Period
石炭二叠纪
1.
Igneous rock intrusion and formation mechanism in coal measures strata of Huabei Permo-Carboniferous Period;
华北石炭二叠纪煤系地层火成岩侵入及形成机制
2.
In order to clarify the time space distribution law of the seams of Permo-Carboniferous Period in Pingdingshan, Yuzhou and Ruzhou Mining Areas, the modern stratigraphy, sedimentology, sequence stratigraphy, and the geophysics exploration theory and method were applied to study of the comparison among the coal measures in the three coalfields.
为了查明平顶山、禹州、汝州矿区石炭二叠纪煤层的时空分布规律,采用现代地层学、沉积学、层序地层学和地球物理勘探学理论和方法研究了3个煤田含煤岩系煤岩层对比。
补充资料:牙形石
牙形石
conodonts
    具有各种各样尖齿或锯齿状物的古代动物遗体,微体古生物学的重要研究内容之一。牙形石个体很小,从不足0.1毫米到约4毫米。未经变质的牙形石一般呈琥珀光泽,浅褐黄、灰白色,透明或不透明。其主要化学成分是磷酸钙,由磷灰石类矿物呈纤维状或薄片状排列而成。牙形石的生物分类位置至今仍未确定。牙形石分布甚广,但仅限于海相沉积物。从寒武纪开始出现,以后几经盛衰,绝灭于三叠纪。牙形石演化十分迅速,为标准化石,用于地层的划分和对比,尤其是井下地层的划分对比起着重要的作用。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条