| Reference Type | Journal (article/letter/editorial) |
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| Title | Anisotropic fragments in strongly folded and faulted coals from the Rocky Mountain area of southeast British Columbia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Goodarzi, Fariborz | Author |
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| Year | 1986 (February 1) | Volume | 23 |
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| Issue | 2 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e86-027Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 478995 | Long-form Identifier | mindat:1:5:478995:0 |
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| GUID | 0 |
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| Full Reference | Goodarzi, Fariborz (1986) Anisotropic fragments in strongly folded and faulted coals from the Rocky Mountain area of southeast British Columbia. Canadian Journal of Earth Sciences, 23 (2) 254-258 doi:10.1139/e86-027 |
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| Plain Text | Goodarzi, Fariborz (1986) Anisotropic fragments in strongly folded and faulted coals from the Rocky Mountain area of southeast British Columbia. Canadian Journal of Earth Sciences, 23 (2) 254-258 doi:10.1139/e86-027 |
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| In | (1986, February) Canadian Journal of Earth Sciences Vol. 23 (2) Canadian Science Publishing |
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| Abstract/Notes | The "Mammoth" coal seam in southeastern British Columbia, Canada, was structurally thickened to 100 m as a result of Laramide folding and faulting. Samples from the coal seam, examined using reflected-light microscopy, include thermally altered coal macerals, their by-products (e.g., pyrolytic carbon), and, in addition, heat-affected preoxidized coke.The heat-affected residues are composed of material formed by friction produced from faulting of the coal-bearing strata. The pyrolytic carbon was formed from the distillation of coal and from coal tar pitch.The occurrence of preoxidized, heat-affected vitrinite suggests that the Mammoth coal seam was oxidized before faulting. |
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