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首页> 外文会议>International Conference on Energy and Environmental Protection >Tectonic Evolution and Coal-bearing Series Hosting Status Analysis on Coal Basins in Eastern Heilongjiang Province in China
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Tectonic Evolution and Coal-bearing Series Hosting Status Analysis on Coal Basins in Eastern Heilongjiang Province in China

机译：中国东部黑龙江省东部煤池的构造演化与煤轴承系列分析

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摘要

The eastern part of Heilongjiang province is an important energy base in northeast Chin;i. with more than fifty small and medium sized coal basins. The article analyzed the relationship between the basins characteristics and the coal-bearing series deposits in this area. In the earh Cretaceous, all the eastern Heilongjiang province area was a large continental margin basin, with the main provenance area located in its west. This makes the coal accumulating effect at that time occi.it> mainly in the west of the near provenance areas, forming the main coal seam in this province. The second major coal accumulating, mainly in rift basins, happened in Paleocene. In late Cretaceous and Paleocene, the former coal accumulating basin was transformed and damaged because of tectonic forces, so that the current coal-bearing series distribution is characterized by isolated small and medium sized coal basins.
机译：黑龙江省东部是东北下的重要能源基础;一世。拥有超过五十个中小型煤池。本文分析了该地区盆地特性与煤轴承系列矿床之间的关系。在耳朵白垩纪，所有东黑龙江省地区都是一个大型大陆边缘盆地，主要出处都位于西方。这使得当时的煤炭积累效应恰好。主要在近乎出处的西部，在这个省形成主煤层。主要在古典上累积的第二个主要煤炭在古代。在晚餐和古典中，由于构造力，以前的煤炭积聚盆地转化和损坏，因此目前的煤串联分布的特点是孤立的中小型煤池。

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