摘要
西伯利亚板块东南缘，从早晚寒武世晚期至早石炭世，地层发育经历了被动陆经、岛孤和弧后盆地、岛弧期后抬升、裂陷槽和陆表海侵期几个阶段，文中详细论述了它们沉积特征及相互关系．
In the southeastern margin region of Siberian plate,from late'Early Cambrian to Early Carboniferous,the stratigraphical development may be divided into passive continental margin,island arc and arc-rear basin,post -island -arc uplift,faulted trough basin and epicontinental progression stages.For these stages,the sedimental characters and their interrelation is detailed in this paper.
出处
《吉林地质》
1996年第3期23-24,共2页
Jilin Geology
关键词
兴安地层区
奥陶纪
岛弧
古生代
志留纪
地层
Hinggan stratigraphical province.Ordovician island arc and arc-rean basim Silurian uplift Devonian faulted trough basin
