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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Bibliographic Details
Published in:International Journal of Coal Geology
Main Authors: Haeri-Ardakani, Omid, Sanei, Hamed
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
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
Arctic
Canada
Canadian Arctic Archipelago
Lambda
Montney
Arctic Archipelago
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
Description
Summary: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.

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