Abstract

Abstract Scanning electron microscopy (SEM) of shales from three unconventional gas/liquid plays (Nordegg, Montney, Duvernay) of the Western Canadian Sedimentary Basin were combined with routine analytical investigations (x-ray diffraction, source rock analyses, mercury porosimetry, and petrography) to characterize mineral composition, mineral assemblage, morphology, organic content, and porosity. The investigations demonstrated that despite marked diagenetic differences between these shales, some common textural and pore characteristics occurred in all samples. The study showed that SEM morphological investigations of unconventional shale reservoirs provided important information about mineral aggregates, cementation, and clay mineral distribution, which allows interpretations about diagenetic history. Combining petrographic analyses with SEM is critical in sediments with pronounced cementation and mineral overgrowth. Conventional secondary electron SEM studies of untreated samples have several advantages over focused ion beam (FIB) milled surfaces as morphological characteristics of larger areas can be evaluated. The study showed that the organic material may not be fully identified, but organic fragments and some bituminous material can still be recognized. In general, abundant large pores (200 to > 2000 nm) can be observed under SEM, but other techniques, such as the mercury porosimetry, failed to identify these larger pores in these shales. The main morphological porosity types in these shales were intergranular (between particles), dissolution, residual growth, fracture, and phyllosilicate pores. The high number of 5- to 20-nm pores as determined by mercury porosimetry could not be confirmed by SEM, which may have been because of resolution issues. Hence, future porosity characterization of gas shales needs to investigate these problems of discrepancy between analytical and imaging technologies.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.