Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator

Geochemical and petrographic effects of burial temperature on sedimentary organic matter have long been recognized and used as various thermal maturity indicators (i.e., pyrolysis T-max, conodont and spore coloration, vitrinite/bitumen/zoodast reflectance), and fluorescent spectrometry (i.e., lambda...

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Published in:International Journal of Coal Geology
Main Authors: Haeri-Ardakani, Omid, Sanei, Hamed
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://pure.au.dk/portal/da/publications/dolomite-fluorescence-redgreen-quotient(a52bf610-1c40-4380-9c25-e726337d0944).html
https://doi.org/10.1016/j.coal.2014.12.005
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spelling ftuniaarhuspubl:oai:pure.atira.dk:publications/a52bf610-1c40-4380-9c25-e726337d0944 2023-05-15T14:28:54+02:00 Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator Haeri-Ardakani, Omid Sanei, Hamed 2015-01-01 https://pure.au.dk/portal/da/publications/dolomite-fluorescence-redgreen-quotient(a52bf610-1c40-4380-9c25-e726337d0944).html https://doi.org/10.1016/j.coal.2014.12.005 eng eng info:eu-repo/semantics/restrictedAccess Haeri-Ardakani , O & Sanei , H 2015 , ' Dolomite fluorescence Red/Green quotient : A potential new thermal maturity indicator ' , International Journal of Coal Geology , vol. 137 , pp. 165-171 . https://doi.org/10.1016/j.coal.2014.12.005 Dolomite fluorescence color Red/Green Quotient Thermal maturity Utica Shale Montney Formation CANADIAN ARCTIC ARCHIPELAGO WEST-CENTRAL ALBERTA CARBONATE PETROGRAPHY DOLOMITIZATION SEDIMENTARY VITRINITE ROCKS BASIN REFLECTANCE GRAPTOLITES article 2015 ftuniaarhuspubl https://doi.org/10.1016/j.coal.2014.12.005 2023-01-04T23:54:46Z Geochemical and petrographic effects of burial temperature on sedimentary organic matter have long been recognized and used as various thermal maturity indicators (i.e., pyrolysis T-max, conodont and spore coloration, vitrinite/bitumen/zoodast reflectance), and fluorescent spectrometry (i.e., lambda(max) and Red/Green quotient). This study investigates variations in the fluorescence color spectra (in the visible light spectrum) of authigenic dolomite over a wide range of thermal maturities. Two sample sets of calcareous shales/siltstones from Eastern and Western Canada, with sparse dolomite crystals in the rock matrix were selected to examine the relationship between thermal maturity and fluorescent properties of dolomite. Results from a range of thermal maturities, from the oil window to the dry gas window, reveal a strong positive correlation between the Red/Green quotient (Q) of dolomite crystals and equivalent vitrinite reflectance (VRo(eqv.)) values. This can be optically described as the color shift in fluorescent properties of dolomite with increasing maturity. This strong positive correlation between Q and thermal maturity can potentially be used as an alternative thermal maturity indicator in calcareous shales with low organic content Compilation of worldwide data is required to understand the relationship trend and conversion equations among dolomite Q and other established thermal maturity indicators. (C) 2014 Elsevier B.V. All rights reserved. Article in Journal/Newspaper Arctic Archipelago Arctic Canadian Arctic Archipelago Aarhus University: Research Arctic Canada Canadian Arctic Archipelago Lambda ENVELOPE(-62.983,-62.983,-64.300,-64.300) Montney ENVELOPE(-120.920,-120.920,56.450,56.450) International Journal of Coal Geology 137 165 171
institution Open Polar
collection Aarhus University: Research
op_collection_id ftuniaarhuspubl
language English
topic Dolomite fluorescence color
Red/Green Quotient
Thermal maturity
Utica Shale
Montney Formation
CANADIAN ARCTIC ARCHIPELAGO
WEST-CENTRAL ALBERTA
CARBONATE PETROGRAPHY
DOLOMITIZATION
SEDIMENTARY
VITRINITE
ROCKS
BASIN
REFLECTANCE
GRAPTOLITES
spellingShingle Dolomite fluorescence color
Red/Green Quotient
Thermal maturity
Utica Shale
Montney Formation
CANADIAN ARCTIC ARCHIPELAGO
WEST-CENTRAL ALBERTA
CARBONATE PETROGRAPHY
DOLOMITIZATION
SEDIMENTARY
VITRINITE
ROCKS
BASIN
REFLECTANCE
GRAPTOLITES
Haeri-Ardakani, Omid
Sanei, Hamed
Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator
topic_facet Dolomite fluorescence color
Red/Green Quotient
Thermal maturity
Utica Shale
Montney Formation
CANADIAN ARCTIC ARCHIPELAGO
WEST-CENTRAL ALBERTA
CARBONATE PETROGRAPHY
DOLOMITIZATION
SEDIMENTARY
VITRINITE
ROCKS
BASIN
REFLECTANCE
GRAPTOLITES
description Geochemical and petrographic effects of burial temperature on sedimentary organic matter have long been recognized and used as various thermal maturity indicators (i.e., pyrolysis T-max, conodont and spore coloration, vitrinite/bitumen/zoodast reflectance), and fluorescent spectrometry (i.e., lambda(max) and Red/Green quotient). This study investigates variations in the fluorescence color spectra (in the visible light spectrum) of authigenic dolomite over a wide range of thermal maturities. Two sample sets of calcareous shales/siltstones from Eastern and Western Canada, with sparse dolomite crystals in the rock matrix were selected to examine the relationship between thermal maturity and fluorescent properties of dolomite. Results from a range of thermal maturities, from the oil window to the dry gas window, reveal a strong positive correlation between the Red/Green quotient (Q) of dolomite crystals and equivalent vitrinite reflectance (VRo(eqv.)) values. This can be optically described as the color shift in fluorescent properties of dolomite with increasing maturity. This strong positive correlation between Q and thermal maturity can potentially be used as an alternative thermal maturity indicator in calcareous shales with low organic content Compilation of worldwide data is required to understand the relationship trend and conversion equations among dolomite Q and other established thermal maturity indicators. (C) 2014 Elsevier B.V. All rights reserved.
format Article in Journal/Newspaper
author Haeri-Ardakani, Omid
Sanei, Hamed
author_facet Haeri-Ardakani, Omid
Sanei, Hamed
author_sort Haeri-Ardakani, Omid
title Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator
title_short Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator
title_full Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator
title_fullStr Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator
title_full_unstemmed Dolomite fluorescence Red/Green quotient:A potential new thermal maturity indicator
title_sort dolomite fluorescence red/green quotient:a potential new thermal maturity indicator
publishDate 2015
url https://pure.au.dk/portal/da/publications/dolomite-fluorescence-redgreen-quotient(a52bf610-1c40-4380-9c25-e726337d0944).html
https://doi.org/10.1016/j.coal.2014.12.005
long_lat ENVELOPE(-62.983,-62.983,-64.300,-64.300)
ENVELOPE(-120.920,-120.920,56.450,56.450)
geographic Arctic
Canada
Canadian Arctic Archipelago
Lambda
Montney
geographic_facet Arctic
Canada
Canadian Arctic Archipelago
Lambda
Montney
genre Arctic Archipelago
Arctic
Canadian Arctic Archipelago
genre_facet Arctic Archipelago
Arctic
Canadian Arctic Archipelago
op_source Haeri-Ardakani , O & Sanei , H 2015 , ' Dolomite fluorescence Red/Green quotient : A potential new thermal maturity indicator ' , International Journal of Coal Geology , vol. 137 , pp. 165-171 . https://doi.org/10.1016/j.coal.2014.12.005
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1016/j.coal.2014.12.005
container_title International Journal of Coal Geology
container_volume 137
container_start_page 165
op_container_end_page 171
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