摘要
江西二叠系可识别出５个三级层序，其中早二叠世３个，晚二叠世２个，它们构筑了２个Ⅰ型层序和３个Ⅱ型层序。与５个层序对应的５个三级海平面升降旋回的速度、幅度和频率均显示出不同的变化特征。
Five third-grade measures can be recognized in the Permian system in Jiangxi,of which three early Permian measures and two Late Permian ones constitute two ltype measures and three Ⅱ-type ones.The speed.amplitude and frequency of five three-grade eustatic cycle corresponing to five measures show different changable features.
出处
《江西地质》
1996年第4期265-273,共9页
Jiangxi Geology
