1991
DOI: 10.1016/0166-5162(91)90014-a
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The relationship between coal petrography and depositional environments from selected coal basins in Canada

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Cited by 128 publications
(78 citation statements)
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“…The second is the neutral use of petrographic data in conjunction with analyses of microfossils (and occasionally macrofossils), ash yield, and mineralogy of coal to develop an integrated picture of trends and parallel patterns in the independent sets of data (e.g.. Smith, 1962;Grady and Eble, 1990). The third is the use of petrographic data alone, usually through the construction of complex indices based on maceral ratios (e.g., Diessel, 1986;Kalkreuth et al, 1991), to infer characteristics of the parental vegetation and mire hydrologic conditions. The first two of these approaches we find promising, empirically based means to estimate mire vegetation and/or environmental conditions.…”
Section: Coal Petrographymentioning
confidence: 99%
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“…The second is the neutral use of petrographic data in conjunction with analyses of microfossils (and occasionally macrofossils), ash yield, and mineralogy of coal to develop an integrated picture of trends and parallel patterns in the independent sets of data (e.g.. Smith, 1962;Grady and Eble, 1990). The third is the use of petrographic data alone, usually through the construction of complex indices based on maceral ratios (e.g., Diessel, 1986;Kalkreuth et al, 1991), to infer characteristics of the parental vegetation and mire hydrologic conditions. The first two of these approaches we find promising, empirically based means to estimate mire vegetation and/or environmental conditions.…”
Section: Coal Petrographymentioning
confidence: 99%
“…Inertinite in general, and fusinite in particular, have been treated as important indicators of "dry" conditions within mires in some petrographically based reconstructions of environments (Hacquebard and Donaldson, 1969;Gelification Index of Diessel, 1982Harvey and Dillon, 1985;Grady and Eble, 1990;Eble and Grady, 1990;Lamberson et al, 1991;Kalkreuth et al, 1991 but not by Calder et al, 1991or Calder, 1993. For fusinite, this inference appears to be based on the assumption that burning is likely to be more frequent in parts of mires with exposed, even if wet, substrates.…”
mentioning
confidence: 99%
“…Several researchers have objected the usage of such indices for Tertiary or low T1 T2 T3 T4 T5 T6 T7 T8 T9 T10 TL1 TL2 TL3 TL4 TL5 TL6 (Bechtel et al 2002(Bechtel et al , 2003(Bechtel et al , 2007a(Bechtel et al , b, 2008Mayr et al 2009;Savard et al 2012;Singh et al 2012c) for the reconstruction of paleoenvironment. Kalkreuth et al (1991), Petersen (1993), andFlores (2002) further modified these indices to make them useful for the low rank coals too. In the present investigation, the indices have been taken from Flores (2002) which is a modified version of Kalkreuth et al (1991), for brown coals.…”
Section: Paleomiresmentioning
confidence: 99%
“…Kalkreuth et al (1991), Petersen (1993), andFlores (2002) further modified these indices to make them useful for the low rank coals too. In the present investigation, the indices have been taken from Flores (2002) which is a modified version of Kalkreuth et al (1991), for brown coals.…”
Section: Paleomiresmentioning
confidence: 99%
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