| 中国东部中生代构造演变与聚煤作用的迁移 |
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| 引用本文： | 陈传诗.中国东部中生代构造演变与聚煤作用的迁移[J].中国煤田地质,1996,8(2):5-8,19. |
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| 作者姓名： | 陈传诗 |
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| 作者单位： | 焦作工学院 |
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| 摘 要： | 中生代期间，中国东部的构造演变具有从西向东不断发展，从南向北不断扩展的特点。正是这种从南向北的构造演变与潮湿气侯带由南向北的不断迁移相结合，决定了中生代聚煤作用不断地从南向北迁移。
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| 关 键 词： | 板块运动 构造演变 聚煤作用 中生代 煤矿床 |
MESOZOIC TECTONIC EVOLUTION AND COAL ACCUMULATION MIGRATION IN THE EASTERN CHINA |
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| Chen Chuanshi.MESOZOIC TECTONIC EVOLUTION AND COAL ACCUMULATION MIGRATION IN THE EASTERN CHINA[J].Coal Geology of China,1996,8(2):5-8,19. |
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| Authors: | Chen Chuanshi |
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| Abstract: | The characteristics of Mesozoic tectonic evolution in the eastern china is developing con-stantly from west to east and spreading consequently from south to nouth. It is because this tectonicevolution combingwith the wet climate zone migration from south to nouth that led to the Mesozoiccoal accumulation migration from south to nouth. |
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| Keywords: | Plate movement tectonic evolution coal accumulation Mesozoic age the eastern china |
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