摘要
依据赣西北东岭剖面上二叠统长兴组上段第5层(厚34.50m)和第8层(厚10.40m)藻海绵生物礁的赋存状况,及其下伏地层(第2层,厚2m;第0层,厚8.20m)所产牙形剌ClarkinachangxingensisClarkinadeflecta组合带的属种特征及其丰度,笔者认为,东岭地区生物礁的形成时代为晚二叠世晚长兴期.
In accordance with the natural endowstates of the algae Sponges reefs,the fifth bed (thickness 34.50 m)and the eighth bed (thickness 10.40 m)at the upper sector of the Changxing formation,in Dongling section of Northwest Jiangxi,and the Genus and Species charcteristics and abundances of the conodonds Clarkina changxingensis Clarkina deflecta assemblage zone at the lower stratum(The second bed,thickness 2 m;the noughth bed,thickness 8.20 m).The Taking Shape Era of the reefs in Dongling Area belong to the late Changxingian of the late Permian.
出处
《江西师范大学学报(自然科学版)》
CAS
1999年第3期252-258,共7页
Journal of Jiangxi Normal University(Natural Science Edition)
基金
江西省自然科学基金
关键词
组合带
晚长兴期
生物礁
东岭剖面
江西
二叠纪
Clarkina changxingensis Clarkina deflecta assemblage zone
the late Changxingian
the reefs
Dongling section
Jiangxi Province