摘要
以松花江地块为基础，论述了早寒武纪世上叠盆地局限海沉积、中奥陶世裂陷火山－沉积及晚古生代三个裂陷槽沉积的地层发育特征。
With Songhuajiang massif as basis,the developing characters of the sediments in Early Cambrian superposed basin, Middle Ordovician faulted volcanic-sedimentary deposits and Late Paleozoic volcanic-Sedimentary deposits in three faulted trough basins are discussed.
出处
《吉林地质》
1996年第3期35-39,共5页
Jilin Geology
关键词
松花江
地层区
古生代
地层
Songhuajiang massif Early Cambrian Middle Ordovician Late Paleozoic Faulted depression Faulted trough basin
