EARLY COALIFICATION FEATURES AS APPROACHED BY SOLID STATE 13C CP/MAS NMR SPECTROSCOPY

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dc.contributor.author Kalaitzidis S.
dc.contributor.author Georgakopoulos A.
dc.contributor.author Christanis K.
dc.contributor.author Iordanidis A.
dc.date.accessioned 2024-08-26T05:22:24Z
dc.date.available 2024-08-26T05:22:24Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=12091926
dc.identifier.citation Geochimica et Cosmochimica Acta, 2006, 70, 4, 947-959
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/44737
dc.description.abstract Solid state 13C CP/MAS NMR spectroscopy and ultimate analysis have been applied to a study of samples from the Pleistocene Drama lignite and its successive modern analogue, the Philippi peat, in northeastern Greece. The succession from peat to lignite resulted in a C enrichment averaging 10.7% and depletion in H and O averaging 6.5 and 18.5%, respectively. Early coalification resulted in the degradation of methoxyl groups, carbohydrates and carboxylic groups, whereas the aliphatic carbons were less affected. However, organic geochemical alteration seems to depend strongly on the initial peatification conditions. The "aromaticity" decreases from the stage of peat to lignite, as a result of the significant degradation of lignin precursors. ? 2005 Elsevier Inc. All rights reserved.
dc.subject COALIFICATION
dc.subject ORGANIC GEOCHEMISTRY
dc.subject SPECTROSCOPY
dc.title EARLY COALIFICATION FEATURES AS APPROACHED BY SOLID STATE 13C CP/MAS NMR SPECTROSCOPY
dc.type Статья
dc.identifier.doi 10.1016/j.gca.2005.10.014
dc.subject.age Кайнозой::Четвертичная::Плейстоцен
dc.subject.age Cenozoic::Quaternary::Pleistocene


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