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Amin Ghanizadeh
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Journal Article

High-resolution petrophysical, geochemical, and geomechanical profiling of a 230-m continuous core from the Montney Formation, Canada

Daniela Becerra, Christopher R. Clarkson, Amin Ghanizadeh
Journal: AAPG Bulletin
Published: 01 March 2024
AAPG Bulletin (2024) 108 (3): 461–478.
DOI: https://doi.org/10.1306/05032322095
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Journal Article

Laboratory-based characterization of pore network and matrix permeability in the Montney Formation: Insights from methodology comparisons

Amin Ghanizadeh, Christopher R. Clarkson, Atena Vahedian, Omid H. Ardakani, James M. Wood, Hamed Sanei
Published: 01 June 2018
Bulletin of Canadian Petroleum Geology (2018) 66 (2): 472–498.
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Journal Article

Introduction to special section: Lacustrine shale characterization and shale resource potential in Ordos Basin, China

Tongwei Zhang, Xiangzeng Wang, Hongliu Zeng, Neil Fishman, Barry J. Katz, Kitty L. Milliken, Mingzhen Wei, Bob Loucks, Amin Ghanizadeh
Journal: Interpretation
Published: 18 April 2017
Interpretation (2017) 5 (2): SFi–SFii.
DOI: https://doi.org/10.1190/INT-2017-0314-SPSEINTRO.1
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Book Chapter

On the Use and Abuse of N 2 Physisorption for the Characterization of the Pore Structure of Shales

Author(s)
Pieter Bertier, Kevin Schweinar, Helge Stanjek, Amin Ghanizadeh, Christopher R. Clarkson, Andreas Busch, Niko Kampman, Dirk Prinz, Alexandra Amann-Hildenbrand, Bernhard M. Krooss, Vitaliy Pipich
Book: Filling the Gaps – from Microscopic Pore Structures to Transport Properties in Shales
Series: Clay Minerals Society Workshop Lectures
Publisher: Clay Minerals Society
Published: 01 January 2016
DOI: 10.1346/CMS-WLS-21-12
EISBN: 9781881208471
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Abstract The use of N 2 physisorption for the characterization of the pore structure of shales is assessed by addressing some common pitfalls and misconceptions related to the interpretation of physisorption data. In addition, N 2 physisorption is compared to other methods used to characterize shales. For this purpose a set of pore-structure and total-porosity data from N 2 physisorption, He-pycnometry, Hg-intrusion porosimetry, fluid saturation (Archimedes) methods, and (ultra) small-angle neutron scattering was obtained from measurements on samples of Opalinus Clay.