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TitleComparison among brittleness, hardness and mineral composition of the Besa River Formation in the Liard Basin, Canada
 
AuthorKim, YORCID logo; Lee, H SORCID logo; Choi, JORCID logo; Kim, K H; Ozyer, C AORCID logo
SourceJournal of Natural Gas Science and Engineering vol. 103, 104632, 2022 p. 1-14, https://doi.org/10.1016/j.jngse.2022.104632 Open Access
logo Open Access
Image
Year2022
Alt SeriesNatural Resources Canada, Contribution Series 20220089
PublisherElsevier B.V.
Documentserial
Lang.English
Mediapaper; digital; on-line
File formatpdf
ProvinceBritish Columbia; Yukon; Northwest Territories
NTS94; 104A; 104H; 104I; 104P; 95A; 95B; 95C; 95D; 105A
Lat/Long WENS-130.0000 -120.0000 61.0000 55.0000
Subjectsgeochemistry; mineralogy; quartz; minerals; Liard Basin; Besa River Formation; Devonian; Mississippian
Illustrationslocation maps; stratigraphic charts; tables; profiles; plots
ProgramEnergy Geoscience
Released2022 05 20
AbstractRock brittleness is regarded as one of the most crucial geomechanical properties affecting hydraulic fracturing in shale reservoirs. Numerous studies have been conducted to quantify rock brittleness, most of which were based on mineralogical and geomechanical properties. This study aims to clarify relationship between brittleness indices and multi-proxies of the Devonian Besa River Formation, which is a frontier shale gas play in Western Canada Sedimentary Basin and to suggest an ideal model for mineralogy-based brittleness index. To this end, we calculated Young's modulus and Poisson's ratio from well logs and measured the Leeb hardness from slabbed core surfaces. We also conducted geochemical and sedimentological analyses for the Besa River Formation. Hardness and brittleness are positively correlated with quartz content but negatively with clay mineral content in the formation, whereas carbonate mineral and total organic carbon (TOC) contents show no relationship with hardness and brittleness. Hardness measurements are also well correlated with rock brittleness from well logs and can be a good proxy for the brittleness of Besa River Formation. This study suggests an ideal model for a mineralogy-based brittleness index, considering the influence of biogenic and detrital quartz in the Formation. This model shows a high correlation coefficient with rock brittleness and can be useful to determine the brittleness of rocks with similar characteristics to Besa River Formation.
Summary(Plain Language Summary, not published)
This study helps clarify the relationship between brittleness indices and multi-proxies of the Devonian Besa River Formation, which is a frontier shale gas play in Western Canada Sedimentary Basin. The study revealed the hardness and brittleness are positively correlated with quartz content but negatively with clay mineral content in the formation, whereas carbonate mineral and total organic carbon (TOC) contents show no relationship with hardness and brittleness. The model in this study shows a high correlation coefficient with rock brittleness and can be useful to determine the brittleness of rocks with similar characteristics to Besa River Formation.
GEOSCAN ID330128

 
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