Organic matter from black shales collected in DSDP Holes 41-367 and 41-368
It is shown that microscopic algae dominate in source material of organic matter of black shales, and admixture of residues of organisms and terrestrial humic material is contained. The main direction of source material transformation during syngenesis and sedimentogenesis is associated with jellofi...
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1978
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.775954 2023-05-15T17:29:28+02:00 Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 Bogolyubova, L I Timofeev, Pyotr P MEDIAN LATITUDE: 14.997000 * MEDIAN LONGITUDE: -20.700500 * SOUTH-BOUND LATITUDE: 12.486800 * WEST-BOUND LONGITUDE: -21.353800 * NORTH-BOUND LATITUDE: 17.507200 * EAST-BOUND LONGITUDE: -20.047200 * DATE/TIME START: 1975-03-03T00:00:00 * DATE/TIME END: 1975-03-13T00:00:00 1978-02-13 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.775954 https://doi.org/10.1594/PANGAEA.775954 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.775954 https://doi.org/10.1594/PANGAEA.775954 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Geological Institute, Russian Academy of Sciences, Moscow Supplement to: Bogolyubova, L I; Timofeev, Pyotr P (1978): Composition of organic matter from black shales of the Cape Verde Basin (Eastern Atlantic) and their oil source potential. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 13(5), 3-17 41-367 41-368 Archive of Ocean Data ARCOD Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg41 North Atlantic/BASIN North Atlantic/CONT RISE Dataset 1978 ftpangaea https://doi.org/10.1594/PANGAEA.775954 2023-01-20T07:32:25Z It is shown that microscopic algae dominate in source material of organic matter of black shales, and admixture of residues of organisms and terrestrial humic material is contained. The main direction of source material transformation during syngenesis and sedimentogenesis is associated with jellofication resulting to formation of organic matter of significantly sapropelic type. Low reflectance of vitrinite and alginite from organic matter refer to the primary and secondary lignite stages of its carbonification. Significantly sapropel type of organic matter and low stage of carbonification are reliable criteria for assigning black shales to the category of potential oil source strata. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-21.353800,-20.047200,17.507200,12.486800) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
41-367 41-368 Archive of Ocean Data ARCOD Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg41 North Atlantic/BASIN North Atlantic/CONT RISE |
spellingShingle |
41-367 41-368 Archive of Ocean Data ARCOD Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg41 North Atlantic/BASIN North Atlantic/CONT RISE Bogolyubova, L I Timofeev, Pyotr P Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 |
topic_facet |
41-367 41-368 Archive of Ocean Data ARCOD Deep Sea Drilling Project DRILL Drilling/drill rig DSDP Glomar Challenger Leg41 North Atlantic/BASIN North Atlantic/CONT RISE |
description |
It is shown that microscopic algae dominate in source material of organic matter of black shales, and admixture of residues of organisms and terrestrial humic material is contained. The main direction of source material transformation during syngenesis and sedimentogenesis is associated with jellofication resulting to formation of organic matter of significantly sapropelic type. Low reflectance of vitrinite and alginite from organic matter refer to the primary and secondary lignite stages of its carbonification. Significantly sapropel type of organic matter and low stage of carbonification are reliable criteria for assigning black shales to the category of potential oil source strata. |
format |
Dataset |
author |
Bogolyubova, L I Timofeev, Pyotr P |
author_facet |
Bogolyubova, L I Timofeev, Pyotr P |
author_sort |
Bogolyubova, L I |
title |
Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 |
title_short |
Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 |
title_full |
Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 |
title_fullStr |
Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 |
title_full_unstemmed |
Organic matter from black shales collected in DSDP Holes 41-367 and 41-368 |
title_sort |
organic matter from black shales collected in dsdp holes 41-367 and 41-368 |
publisher |
PANGAEA |
publishDate |
1978 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.775954 https://doi.org/10.1594/PANGAEA.775954 |
op_coverage |
MEDIAN LATITUDE: 14.997000 * MEDIAN LONGITUDE: -20.700500 * SOUTH-BOUND LATITUDE: 12.486800 * WEST-BOUND LONGITUDE: -21.353800 * NORTH-BOUND LATITUDE: 17.507200 * EAST-BOUND LONGITUDE: -20.047200 * DATE/TIME START: 1975-03-03T00:00:00 * DATE/TIME END: 1975-03-13T00:00:00 |
long_lat |
ENVELOPE(-21.353800,-20.047200,17.507200,12.486800) |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Geological Institute, Russian Academy of Sciences, Moscow Supplement to: Bogolyubova, L I; Timofeev, Pyotr P (1978): Composition of organic matter from black shales of the Cape Verde Basin (Eastern Atlantic) and their oil source potential. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 13(5), 3-17 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.775954 https://doi.org/10.1594/PANGAEA.775954 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.775954 |
_version_ |
1766123602938167296 |