摘要
在生物地层及年代地层研究的基础上,对本区上石炭统至中二叠统进行了层序地层学研究,从船山组至孤峰组下部共划分了5个三级层序、13个四级层序。通过五百多个米级旋回层序的研究,认为本区海盆有台地、台盆相间及盆地3个发展阶段,并得出4—6个米级旋回层序组成一个更高级别旋回的结论。
Based on the biostratigraphic and chronostratigraphic data,the Carboniferous-Permian strata (from the Chuanshan Formation to the Gufeng Formation) in the Tonglu region of Zhejiang Province can be divided into five third-order sequences and 13 fourth-order sequences. In general, 4-6 meter-scale parasequences make a sequence of higher order. Sequence stratigraphic data also indicate that the 500-mthick Carboniferous-Permian succession in the Tonglu region represent a deepening upward sequence,beginning in platform facies and in deep water basinal facies.
出处
《地层学杂志》
CSCD
北大核心
2007年第1期90-97,共8页
Journal of Stratigraphy
基金
中国地质调查局1/25万<金华市幅>国土资源大调查项目(200113000032)资助
关键词
三级层序
米级旋回层序
层序地层学
桐庐
浙江
石炭系
二叠系
Tonglu, Zhejiang, third-order sequence, meter-scale parasequence, sequence-stratigraphy, Carboniferous, Permian