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Notes on the origin of inertinite macerals in coals: Observations on the importance of fungi in the origin of macrinite

  • James C. Hower
  • , Jennifer M.K. O'Keefe
  • , Michael A. Watt
  • , Timothy J. Pratt
  • , Cortland F. Eble
  • , J. D. Stucker
  • , Allison R. Richardson
  • , Irena J. Kostova

Producción científica: Articlerevisión exhaustiva

94 Citas (Scopus)

Resumen

Macrinite is a, generally, rare inertinite maceral, often incorporating remnants and fragments of other macerals, including vitrinite, liptinite, and other inertinite. The associated inertinites include multiple forms of funginite. Funginite is also commonly found in association with vitrinite of slightly elevated reflectance and with degraded varieties of vitrinite. Together with the highly degraded macrinite, the latter two associations are here inferred to be part of a continuum of fungal and microbial degradation of peat. In any case, the origin of some macrinite is potentially distinct from that of inertinite generated by fire.

Idioma originalEnglish
Páginas (desde-hasta)135-143
Número de páginas9
PublicaciónInternational Journal of Coal Geology
Volumen80
N.º2
DOI
EstadoPublished - nov 1 2009

ASJC Scopus subject areas

  • Fuel Technology
  • Geology
  • Economic Geology
  • Stratigraphy

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