| 兴安地层区的古生代地层 |
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| 引用本文： | 苏养正.兴安地层区的古生代地层[J].吉林地质,1996(Z1). |
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| 作者姓名： | 苏养正 |
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| 作者单位： | 地矿部沈阳地质矿产研究所 |
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| 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．
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| 关 键 词： | 兴安地层区，奥陶纪，岛弧及弧后，志留纪，期后抬升，泥盆纪，裂陷槽 |
PALEOZOIC STRATIGRAPHY OF HINGGAN STRATIGRAPHICAL PROVINCE |
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| Su Yangzheng.PALEOZOIC STRATIGRAPHY OF HINGGAN STRATIGRAPHICAL PROVINCE[J].Jilin Geology,1996(Z1). |
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| Authors: | Su Yangzheng |
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| Abstract: | 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. |
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| Keywords: | Hinggan stratigraphical province Ordovician island arc and arc-rean basim Silurian uplift Devonian faulted trough basin |
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