1) Carboniferous~Pernian ice age
石炭-二叠纪冰川
2) Permo-Calrboniferous glacial period
石炭-二叠纪冰期
3) 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
4) 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。
5) 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。
6) Carbono-Permian coal series
石炭-二叠纪煤系
1.
Hydrocarbon generation and evolution of Carbono-Permian coal series from the Well Su-50 in the Wuqing Sag,Central Hebei Depression;
冀中坳陷武清凹陷苏50井石炭-二叠纪煤系的成烃演化
补充资料:二叠纪三叠纪灭绝事件
二叠纪-三叠纪灭绝事件,是发生在大约2亿5,200万年前二叠纪和三叠纪交替时期的生物集群灭绝事件。
这一事件导致了70%的陆生物种和90%的海洋物种灭绝。古生代海洋中由海百合-腕足动物-苔藓虫组成的表生、固着生物群落迅速退出历史舞台,为中生代由现代软体动物-甲壳动物-硬骨鱼构成的内生、移动生物群落的崛起创造了条件。
有多种理论解释了灭绝的原因,包括:
撞击事件
板块构造
超新星
火山作用
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