Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland

journal article Nine samples of oil shale from the Carboniferous Rocky Brook Formation along Rocky Brook in western Newfoundland were studied by incident light microscopy and geochemical analysis (Rock-Eval pyrolysis) to determine the maceral components, geochemical type, and maturation level of the...

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Main Author: Kalkreuth, W.; Macauley, G.
Language:English
Published: Canadian Society of Petroleum Geologists 1989
Subjects:
Online Access:https://collections.lib.utah.edu/ark:/87278/s6wt1sfk
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spelling ftunivutah:oai:collections.lib.utah.edu:ir_eua/214672 2023-05-15T17:22:23+02:00 Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland Kalkreuth, W.; Macauley, G. 1989-03 https://collections.lib.utah.edu/ark:/87278/s6wt1sfk eng eng Canadian Society of Petroleum Geologists Bulletin of Canadian Petroleum Geology; vol. 37, no. 1, March, pp. 31-42 (1989) https://collections.lib.utah.edu/ark:/87278/s6wt1sfk organic petrology rock-eval studies oil shales Lower Carboniferous Rocky Brook Formation microscopy and geochemical analysis rock-eval pyrolysis 1989 ftunivutah 2021-06-03T18:21:51Z journal article Nine samples of oil shale from the Carboniferous Rocky Brook Formation along Rocky Brook in western Newfoundland were studied by incident light microscopy and geochemical analysis (Rock-Eval pyrolysis) to determine the maceral components, geochemical type, and maturation level of the kerogen fraction, and to determine the character and potential yield of the pyrolyzate. These oil shale beds are Type I lacustrine lamosites dominated by the maceral lamalginite. Optical properties indicate low to moderate thermal maturation but, as shown by geochemical analyses, the beds are immature and hydrocar- bons have not yet been generated. This relationship is characteristic of Type I deposits. The laminated strata generally contain greater than 5% organic carbon and yield upon pyrolysis sufficient petroleum product to be of economic interest; however, known bed thicknesses are too low to be currently attractive. More massive organic-rich beds may contain less than 4% organic carbon; the yield potential in these beds is severely restricted by an apparent mineral-matrix effect. Other/Unknown Material Newfoundland The University of Utah: J. Willard Marriott Digital Library
institution Open Polar
collection The University of Utah: J. Willard Marriott Digital Library
op_collection_id ftunivutah
language English
topic organic petrology
rock-eval studies
oil shales
Lower Carboniferous Rocky Brook Formation
microscopy and geochemical analysis
rock-eval pyrolysis
spellingShingle organic petrology
rock-eval studies
oil shales
Lower Carboniferous Rocky Brook Formation
microscopy and geochemical analysis
rock-eval pyrolysis
Kalkreuth, W.; Macauley, G.
Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland
topic_facet organic petrology
rock-eval studies
oil shales
Lower Carboniferous Rocky Brook Formation
microscopy and geochemical analysis
rock-eval pyrolysis
description journal article Nine samples of oil shale from the Carboniferous Rocky Brook Formation along Rocky Brook in western Newfoundland were studied by incident light microscopy and geochemical analysis (Rock-Eval pyrolysis) to determine the maceral components, geochemical type, and maturation level of the kerogen fraction, and to determine the character and potential yield of the pyrolyzate. These oil shale beds are Type I lacustrine lamosites dominated by the maceral lamalginite. Optical properties indicate low to moderate thermal maturation but, as shown by geochemical analyses, the beds are immature and hydrocar- bons have not yet been generated. This relationship is characteristic of Type I deposits. The laminated strata generally contain greater than 5% organic carbon and yield upon pyrolysis sufficient petroleum product to be of economic interest; however, known bed thicknesses are too low to be currently attractive. More massive organic-rich beds may contain less than 4% organic carbon; the yield potential in these beds is severely restricted by an apparent mineral-matrix effect.
author Kalkreuth, W.; Macauley, G.
author_facet Kalkreuth, W.; Macauley, G.
author_sort Kalkreuth, W.; Macauley, G.
title Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland
title_short Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland
title_full Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland
title_fullStr Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland
title_full_unstemmed Organic petrology and rock-eval studies on oil shales from the Lower Carboniferous Rocky Brook Formation, Western Newfloundland
title_sort organic petrology and rock-eval studies on oil shales from the lower carboniferous rocky brook formation, western newfloundland
publisher Canadian Society of Petroleum Geologists
publishDate 1989
url https://collections.lib.utah.edu/ark:/87278/s6wt1sfk
genre Newfoundland
genre_facet Newfoundland
op_relation Bulletin of Canadian Petroleum Geology; vol. 37, no. 1, March, pp. 31-42 (1989)
https://collections.lib.utah.edu/ark:/87278/s6wt1sfk
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