- Research Article
1
- 10.1021/acsomega.4c03320
Petrographic andMolecular Characterization of Organic-RichMudstones with Petroleum Generative Potential from The Lower TriassicMontney Formation, Western Canada
- Nov 25, 2024
- ACS Omega
- Daniela Becerra + 5 more +5
The Triassic MontneyFormation hosts major oil and gas resourcesin Western Canada. Despite significant historical development of theseresources, the origin of its hydrocarbons remains unclear, partlydue to limited evidence of primary organic matter within the formation.Most of the hydrocarbons in the Triassic Montney Formation are trappedin low-permeability siltstone facies. For the purposes of this study,however, we investigated the lesser-known and understudied organic-and clay-rich mudstone beds, typically ranging from 2 to 8 cm in thickness,which are interbedded with the siltstone reservoir facies. Petrographicand organic geochemical analyses were conducted on core samples froma well located in west-central Alberta with thermal maturity of 0.95–1.16%Ro.Petrographic analysis, including kerogen maceral composition and fluorescenceof petroleum fluid inclusions, reveals that the organic matter inthe Montney Formation is closely linked to its host lithology. Organic-richmudstone facies, with TOC values up to 3.5 wt %, contain primary kerogen(32–74 vol %) and solid bitumen (29–68 vol %). In contrast,the more organic-lean siltstone facies (TOC < 0.8 wt %) containprimarily pore-filling solid bitumen and lack structured kerogen.Kerogen within the organic-rich mudstone facies is mainly composedof liptinite macerals, including amorphinite, liptodetrinite, andalginite, subordinate amounts of acritarch and sporinite, and tracesof inertinite and vitrinite macerals. The primary organic matter inthe mudstone facies is presumed to be derived from marine sources(i.e., phytoplanktonic algae and bacterial biomass). Its preservationmay result from the balance between periodic high productivity (potentiallydriven by river floods), rapid sedimentation to bury and preserveorganic matter, and low dilution by siliciclastic material. Organicpetrology analysis suggests an in situ generation of hydrocarbonsin the mudstone beds and a potential subsequent short-distance migrationto adjacent siltstone beds. Biomarker analysis supports the geneticlinkage between rock extracts from these beds. Additionally, threefamilies of petroleum fluid inclusions were systematically observed(using fluorescence microscopy) in several sets of contiguous siltstoneand mudstone beds. These findings suggest that the organic-rich mudstonefacies partially contributed to the present-day hydrocarbons of theMiddle Montney Member in the study area.
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