| 湘中涟源下石炭统的陆源碎屑风暴岩 |
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| 引用本文： | 邵龙义,张鹏飞.湘中涟源下石炭统的陆源碎屑风暴岩[J].煤田地质与勘探,1990,18(6):16-19. |
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| 作者姓名： | 邵龙义 张鹏飞 |
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| 作者单位： | 中国矿业大学北京研究生部 |
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| 摘 要： | 描述了测水组具丘状层理的石英砂岩风暴岩和具丘状层理的粉砂岩风暴岩以及邵东组的具粒序层理的粉砂质风暴岩和泥质介壳层风暴岩,四种风暴岩的环境分布依次为前滨——上临滨、下临滨——过渡带、远滨或滨外泥质陆棚。
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| 关 键 词： | 碎屑 风暴岩 陆源 早石炭世 |
THE CLASTIC TEMPESTITES IN LOWER CARBONIFROUS OF CENTRAL HUNAN |
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| Abstract: | The clastic tempestites in Lower Carboniferous Shaodong and Ceshui Formations are first reported.The tempestites in Ceshui Formation consist of quartz arenites and siltstones with the hummocky cross stratification,and in Shaodong Formation consit of siltstones and muddy shell beds with the ripple lamination and graded bedding.They were formed in the foreshore shoreface and offshore muddy shelf environments. |
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