| 大兴安岭─燕山地层分区中、新生代地层 |
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| 引用本文： | 刘尔义.大兴安岭─燕山地层分区中、新生代地层[J].吉林地质,1996(Z1). |
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| 作者姓名： | 刘尔义 |
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| 作者单位： | 地矿部吉林地勘局区调所 |
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| 摘 要： | 对大兴安岭和燕山北部的中生代地层，进行了系统的总结。侏罗纪早中期为含煤地层，晚期为以兴安岭群为代表的火山堆积；白垩纪早期为火山－沉积含煤地层，晚期为红层。第三纪以二连盆地合大量哺乳动物群的杂色沉积为特征。
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| 关 键 词： | 大兴安岭，兴安岭群，热河群，红层 |
MESO-CENOZOIC STRATIGRAPHY IN DA HINGGAN LING-YANSHAN STRATIGRAPHYCAL SUBPROVINCE |
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| Liu Eryi.MESO-CENOZOIC STRATIGRAPHY IN DA HINGGAN LING-YANSHAN STRATIGRAPHYCAL SUBPROVINCE[J].Jilin Geology,1996(Z1). |
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| Authors: | Liu Eryi |
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| Abstract: | The Mesozoic stratigraphy of Da HingganLing- Yianshan stratigraphical subprovince are systemetically summed up, The Early Middle Jurassic is characterized by coal -bearing strata, the Late Jurassic by volcanic accumulation represented by Hingganling group,Early Cretaceous by coal -bearing volcnic - sedimentary rocks and Late Cretaceous by red beds.The Tertiary is represented by varicolored deposits yeilding a great deal of mammal fossils in Eren basin. |
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| Keywords: | Da Hingan Ling Hingganling Group Rehe Group Red beds |
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