Petrographic maturity parameters of a Devonian shale maturation series, Appalachian Basin, USA. ICCP Thermal Indices Working Group interlaboratory exercise

• Type: Article in International Scientific Journal
• Date: 2014

Authors

Carla Viviane Araujo (Author) Other; Angeles G Borrego (Author) Other; Brian Cardott (Author) Other; Renata Brenand A das Chagas (Author) Other; Deolinda Flores (Author) FCUP; Paula Goncalves (Author) FCUP; Paul C Hackley (Author) Other; James C Hower (Author) Other; Marcio Luciano Kern (Author) Other; Jolanta Kus (Author) Other; Maria Mastalerz (Author) Other; Joao Graciano Mendonca Filho (Author) Other; Joalice de Oliveira Mendonca (Author) Other; Taissa Rego Menezes (Author) Other; Jane Newman (Author) Other; Isabel Suarez Ruiz (Author) Other; Frederico Sobrinho da Silva (Author) Other; Igor Viegas de Souza (Author) Other

Journal

Title: International Journal of Coal Geology

Vol. 130

Pages: 89-101

ISSN: 0166-5162

Publisher: Elsevier

Indexing

ISI Web of Knowledge - 29 Citations

Scopus - 32 Citations

Scientific classification

FOS: Engineering and technology > Environmental engineering

Other information

Authenticus ID: P-009-PWD

DOI: 10.1016/j.coal.2014.05.002

Abstract (EN): This paper presents results of an interlaboratory exercise on organic matter optical maturity parameters using a natural maturation series comprised by three Devonian shale samples (Huron Member, Ohio Shale) from the Appalachian Basin, USA. This work was conducted by the Thermal Indices Working Group of the International Committee for Coal and Organic Petrology (ICCP) Commission II (Geological Applications of Organic Petrology). This study aimed to compare: 1. maturation predicted by different types of petrographic parameters (vitrinite reflectance and spectral fluorescence of telalginite), 2. reproducibility of the results for these maturation parameters obtained by different laboratories, and 3. improvements in the spectral fluorescence measurement obtained using modem detection systems in comparison with the results from historical round robin exercises. Mean random vitrinite reflectance measurements presented the highest level of reproducibility (group standard deviation 0.05) for low maturity and reproducibility diminished with increasing maturation (group standard deviation 0.12). Corrected fluorescence spectra, provided by 14 participants, showed a fair to good correspondence. Standard deviation of the mean values for spectral parameters was lowest for the low maturity sample but was also fairly low for higher maturity samples. A significant improvement in the reproducibility of corrected spectral fluorescence curves was obtained in the current exercise compared to a previous investigation of Toarcian organic matter spectra in a maturation series from the Paris Basin. This improvement is demonstrated by lower values of standard deviation and is interpreted to reflect better performance of newer photo-optical measuring systems. Fluorescence parameters measured here are in good agreement with vitrinite reflectance values for the least mature shale but indicate higher maturity than shown by vitrinite reflectance for the two more mature shales. This red shift in lambda(max) beyond 0.65% vitrinite reflectance was also observed in studies of Devonian shale in other basins, suggesting that the accepted correlation for these two petrographic thermal maturity parameters needs to be re-evaluated. A good linear correlation between lambda(max) and T-max for this maturation series was observed and lambda(max) 600 nm corresponds to Tmax of 440 degrees C. Nevertheless if a larger set of Devonian samples is included, the correlation is polynomial with a jump in lambda(max) ranging from 540 to 570 nm. Up to 440 degrees C of T-max, the lambda(max), mostly, reaches up to 500 nm; beyond a T-max of 440 degrees C, lambda(max) is in the range of 580-600 nm. This relationship places the "red shift" when the onset of the oil window is reached at T-max of 440 degrees C. Moreover, the correlation between HI and lambda(max) (r(2) = 0.70) shows a striking inflection and decrease in HI above a lambda(max) of 600 nm, coincident with the approximate onset of hydrocarbon generation in these rocks.

Language: English

Type (Professor's evaluation): Scientific

No. of pages: 13