Organic petrology as a tool for peat-forming environmental reconstructions: insights from Suhostrel and Bobov Dol coals, SW Bulgaria

A. Zdravkov, Doris Groβ, D. Životić, Ivan Kojić, K. Stojanović, Achim Bechtel
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Abstract

The petrographic composition of samples from Suhostrel and Bobov Dol coal deposits was studied using optical micro­scopy. The maceral contents were further used to calculate maceral ratios which were interpreted in terms of environmental condition during peat deposition. Petrographic data of Suhostrel coal is compatible with its organic geochemical characteristics and indicate peat formation under inundated topogenous, meso- to rheotropic, sparsely forested marsh- or fen-type environment. Coal facies diagrams for Bobov Dol coal, however, provide contradictory depositional settings and therefore cannot be used alone for environmental reconstruction.
有机岩石学作为泥炭形成环境重建的工具:保加利亚西南部 Suhostrel 和 Bobov Dol 煤炭的启示
使用光学显微镜研究了 Suhostrel 和 Bobov Dol 煤层样本的岩相组成。大分子含量被进一步用来计算大分子比率,并根据泥炭沉积过程中的环境条件进行解释。Suhostrel 煤的岩相数据与其有机地球化学特征相符,表明泥炭是在淹没的地表、中到流变、疏林沼泽或沼泽型环境中形成的。然而,Bobov Dol 煤的煤层面图提供了相互矛盾的沉积环境,因此不能单独用于环境重建。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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