1) Carbonic-Devonian
石炭-泥盆系
1.
The study result of the seismic 3D data interpretation in the east area of Near Caspian Sea basin shows that on the east and west sides of the tableland hinge zone,there are many regular seismic abnormity events of the Carbonic-Devonian organic reefs.
在对滨里海盆地东缘KJ地区的三维地震资料作常规解释中发现:台地东、西两侧枢纽地带的石炭-泥盆系分布有规律性较强的地震异常。
2) C/D boundary
泥盆-石炭系界线
3) the Neodevonian Carboniferous
晚泥盆世-石炭纪
4) Devonian-Carboniferous
泥盆纪-石炭纪
5) from the end of Devonian Period to early Carboniferous epoch
泥盆纪末至早石炭世
1.
According to data of 1∶50 000 regional geological survey of Northern Guangxi, the biota from the end of Devonian Period to early Carboniferous epoch was summarized, a lot of biozones was classified: there are 12 foram Zones, 11 Anthozoa Zones, 6 Brachiopoda Zones, 5 Conodont Zone, 2 ammonites Zones and 2 Ostracoda Zones, the suggestions for classification of chronostratigraphic is also proposed.
文章根据近年桂北地区 1∶5万区域地质调查和专题研究成果 ,对泥盆纪末至早石炭世生物群作了较系统的总结 ,划分了若干可与区域乃至世界对比的生物 (组合 )带 :有孔虫 12个 ,珊瑚 11个 ,腕足类 6个 ,牙形刺 5个 ,菊石、介形类各 2个 ;并提出了年代地层划分的意
6) late Devonian-early Carboniferous
晚泥盆世-早石炭世
补充资料：泥盆系
见泥盆纪。
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