Dimitrios Charlaftis dimitrios.charlaftis@durham.ac.uk
Academic Visitor
Experimental study of chlorite authigenesis and influence on porosity maintenance in sandstones
Charlaftis, D; Jones, S.J; Dobson, K.J; Crouch, J; Acikalin, S
Authors
Dr Stuart Jones stuart.jones@durham.ac.uk
Associate Professor
K.J Dobson
J Crouch
S Acikalin
Abstract
Chlorite is recognized as a key mineral for preserving reservoir quality in deeply buried sandstones, as chlorite coatings inhibit the nucleation of quartz overgrowths. A limited understanding of the mechanisms and conditions under which these authigenic chlorite coatings form prevents the accurate forward modeling of diagenesis and limits reservoir quality models critical to a wide range of geoscience applications. We present experimental data that show how authigenic chlorite grain coatings preserve porosity in deeply buried sandstone reservoirs, using a series of hydrothermal reactor experiments to simulate quartz cementation and capture the evolving porosity. To simulate reservoir evolution, berthierine-bearing sandstone samples (Lower Jurassic Cook Formation, Oseberg Field, 30/6-17R, Norway) were exposed to a silica-supersaturated Na2CO3 (0.1 M) solution for 72 hours at temperatures of between 100 and 250 °C. Quantification of the temperature-dependent changes in the volume of authigenic chlorite, the thickness and coverage of the clay coatings, and the sample porosity shows increases in chlorite volume (from ∼ 2% to ∼ 14%). This occurs by the transformation, of patchy amorphous berthierine into grain-coating Fe-chlorite cements through a mixture of the solid-state transformation and dissolution–precipitation mechanisms, siderite replacement, and direct precipitation on clay-free surfaces. With increasing temperature, the chlorite coatings increase from ∼ 3.8 μm to ∼ 5.4 μm thick and expand their grain surface coverage from ∼ 28% to ∼ 50%. The face-to-edge and face-to-face foliaceous structure of the clay coatings produced are morphologically similar to those observed in deeply buried sandstones. Only above temperatures of 175 °C is porosity preserved as a consequence of inhibition of quartz overgrowths and the generation of secondary porosity.
Citation
Charlaftis, D., Jones, S., Dobson, K., Crouch, J., & Acikalin, S. (2021). Experimental study of chlorite authigenesis and influence on porosity maintenance in sandstones. Journal of Sedimentary Research, 91(2), 197-212. https://doi.org/10.2110/jsr.2020.122
Journal Article Type | Article |
---|---|
Acceptance Date | Dec 21, 2020 |
Online Publication Date | Mar 25, 2021 |
Publication Date | 2021 |
Deposit Date | Feb 4, 2021 |
Publicly Available Date | Nov 15, 2021 |
Journal | Journal of Sedimentary Research |
Print ISSN | 1527-1404 |
Publisher | Society for Sedimentary Geology (SEPM) |
Peer Reviewed | Peer Reviewed |
Volume | 91 |
Issue | 2 |
Pages | 197-212 |
DOI | https://doi.org/10.2110/jsr.2020.122 |
Public URL | https://durham-repository.worktribe.com/output/1247007 |
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Accepted Journal Article
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Copyright Statement
Accepted for publication in Journal of Sedimentary Research as of 21 December 2020.
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