49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF
LECO analysis, pyrolysis assay, and bitumen and elemental analysis were used to characterize the organic matter of 23 black shale samples from Deep Sea Drilling Project Leg 93, Hole 603B, located in the western North Atlantic. The organic matter is dominantly gas-prone and/or refractory. Two cores w...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.611.8322 2023-05-15T17:31:48+02:00 49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF Selected Black Shales Barry J. Katz The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.611.8322 http://www.deepseadrilling.org/93/volume/dsdp93_49.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.611.8322 http://www.deepseadrilling.org/93/volume/dsdp93_49.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.deepseadrilling.org/93/volume/dsdp93_49.pdf text ftciteseerx 2016-01-08T14:33:07Z LECO analysis, pyrolysis assay, and bitumen and elemental analysis were used to characterize the organic matter of 23 black shale samples from Deep Sea Drilling Project Leg 93, Hole 603B, located in the western North Atlantic. The organic matter is dominantly gas-prone and/or refractory. Two cores within the Turonian and Cenomanian, however, contained significant quantities of well-preserved, hydrogen-enriched, organic matter. This material is thermally imma-ture and represents a potential oil-prone source rock. These sediments do not appear to have been deposited within a stagnant, euxinic ocean as would be consistent with an "oceanic anoxic event. " Their organic geochemical and sedi-mentary character is more consistent with deposition by turbidity currents originating on the continental shelf and slope. Text North Atlantic Unknown |
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ftciteseerx |
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English |
description |
LECO analysis, pyrolysis assay, and bitumen and elemental analysis were used to characterize the organic matter of 23 black shale samples from Deep Sea Drilling Project Leg 93, Hole 603B, located in the western North Atlantic. The organic matter is dominantly gas-prone and/or refractory. Two cores within the Turonian and Cenomanian, however, contained significant quantities of well-preserved, hydrogen-enriched, organic matter. This material is thermally imma-ture and represents a potential oil-prone source rock. These sediments do not appear to have been deposited within a stagnant, euxinic ocean as would be consistent with an "oceanic anoxic event. " Their organic geochemical and sedi-mentary character is more consistent with deposition by turbidity currents originating on the continental shelf and slope. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Selected Black Shales Barry J. Katz |
spellingShingle |
Selected Black Shales Barry J. Katz 49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF |
author_facet |
Selected Black Shales Barry J. Katz |
author_sort |
Selected Black Shales |
title |
49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF |
title_short |
49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF |
title_full |
49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF |
title_fullStr |
49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF |
title_full_unstemmed |
49. ORGANIC GEOCHEMICAL CHARACTER AND HYDROCARBON SOURCE POTENTIAL OF |
title_sort |
49. organic geochemical character and hydrocarbon source potential of |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.611.8322 http://www.deepseadrilling.org/93/volume/dsdp93_49.pdf |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://www.deepseadrilling.org/93/volume/dsdp93_49.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.611.8322 http://www.deepseadrilling.org/93/volume/dsdp93_49.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766129577490382848 |