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云南第三纪白泡煤的成煤植物及煤的成因
引用本文:王士俊,于冰.云南第三纪白泡煤的成煤植物及煤的成因[J].煤炭学报,1997,22(1):8-12.
作者姓名:王士俊  于冰
作者单位:[1]中国科学院植物研究所 [2]中国矿业大学
摘    要:通过对云南金所盆地和潦许盆地晚第三纪浅色褐煤(白泡煤)中植物残体的详细研究,认为白泡煤不是由煤炭藓植物形成,而主要是由松柏类和被子植物形成,其中草本被子植物可能起着比较重要的作用。由成煤植物所反映的古气候条件,白泡煤也不是在干燥或氧化的环境中形成,而可能是在相当潮湿的环境中形成的。

关 键 词:植物残体  成煤植物  白泡煤  煤矿床  成因

COAL FORMING PLANTS OF TERTIARY BAIPAOMEICOAL IN YUNNAN AND ITS GENESIS
Wang Shijun.COAL FORMING PLANTS OF TERTIARY BAIPAOMEICOAL IN YUNNAN AND ITS GENESIS[J].Journal of China Coal Society,1997,22(1):8-12.
Authors:Wang Shijun
Abstract:A detailed study of the phyteral of the Late Tertiary light lignite (Baipaomei coal) from Jinsuo Basin and Liaohu Basin in Yunnan Province is made. It is considered that the Baipaomei coal is formed mainly by conifers and angiosperms,and in the angiosperms herbs might have played an important role,instead of sphagnum.Baipaomei coal was formed in rather damp environment,not in a dry or oxidizing environment.
Keywords:phyteral  coal  forming plants  Baipaomei coal  genesis of coal
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