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Palynological and petrographical reconstruction of peat accumulation in the Trans-Carpathians and in the Pannonian Basin at Ilnitsa and Visonta coalfields

机译:伊尔尼察和维森塔煤田跨喀尔巴阡山脉和潘诺尼亚盆地泥炭堆积的孢粉学和岩石学重建

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摘要

The study of petrographic composition, quality, and spore and pollen complexes of brown coals allows the reconstruction of palaeoconditions of peat accumulation at Ilnitsa and Visonta coalfields. The objective of this research is to provide comparative characteristics of Late Miocene - Pliocene coals in the Trans-Carpathians (Ukraine) and in the Great Hungarian Plain (Hungary) to reconstruct the accumulation conditions in the palaeopeat-bogs by petrographic composition, proximal analysis and palynological data. The results show the predominance of the vitrinite group, in average 79% of the organic substances for Ilnitsa and 86% - for Visonta. The liptinite content is 14% (Ilnitsa) and 10% (Visonta); the inertinite content is 7% and 4%, accordingly. The mineral component amounts are ranging from 1 to 29% in Ilnitsa coals and from 11 to 19% in Visonta. The presence of admixtures of tuff material and opal in the mineral matter are typical in the Ilnitsa coals.
机译:对褐煤的岩石学组成,质量以及孢子和花粉复合物的研究使Ilnitsa和Visonta煤田的泥炭堆积古环境得以重建。本研究的目的是提供跨喀尔巴阡山脉(乌克兰)和匈牙利大平原(匈牙利)中晚新世-上新世煤的对比特征,以通过岩相组成,近端分析和孢粉学数据。结果表明,镜质组占优势,伊利尼察平均占79%,Visonta平均占86%。锂皂石的含量为14%(伊尼莎)和10%(维森塔);惰质含量分别为7%和4%。 Ilnitsa煤中的矿物成分含量为1%至29%,Visonta中的矿物成分含量为11%至19%。 Ilnitsa煤中典型的是在矿物质中存在凝灰岩材料和蛋白石的混合物。

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