Origin and distribution of grain-coating and pore-filling chlorite in deltaic sandstones for reservoir quality assessment



Griffiths, Joshua, Worden, Richard ORCID: 0000-0002-4686-9428, Utley, James ORCID: 0000-0003-0397-5607, Brostrom, Christian, Martinius, Allard, Lawan, Auwala and Al-Hajri, Ali
(2021) Origin and distribution of grain-coating and pore-filling chlorite in deltaic sandstones for reservoir quality assessment. Marine and Petroleum Geology, 134. p. 105326.

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Abstract

Grain-coating chlorite preserves porosity and permeability through the inhibition of quartz cement whereas pore-filling chlorite blocks pore-throats and diminishes reservoir quality. The aim of this study is to determine the origin and principal mechanisms which govern the distribution of grain-coating and pore-filling chlorite in Jurassic deltaic sandstones (Tilje Formation, Smørbukk field, Mid Norwegian Shelf). The study focussed on very high-density sampling for petrographic analysis, from three sections of sandstone core from the same well with contrasting reservoir quality, rather than the low-density sampling approach typically employed. The aim was to gain new understanding of specific controls on porosity and permeability based on core description, porosity and permeability measurements and a suite of petrographic techniques. Results of this study show grain-coating chlorite originated from the thermally-driven recrystallisation of detrital clay coats and/or clay mineral precursors. Pore-filling chlorite has principally derived from the ductile deformation of chlorite-rich Fe-ooids, that were possibly reworked from an evaporitic setting. The distribution of chlorite precursor material, detrital clay coats, and subsequently the distribution of grain-coating and pore-filling chlorite, were controlled by the relative dominance of tidal and fluvial processes active during sediment deposition. Optimum grain-coating chlorite is found in tidal-fluvial sandstones with moderate fluvial influence. Pore-filling chlorite is pervasive in tidal-fluvial channel sandstones deposited during periods of high fluvial discharge, or proximal to the central turbidity maximum zone; marked by an abundance of fluid mud. Tidal channel sandstones with no fluvial influence are pervasively quartz cemented due to an absence of grain-coating chlorite. Grain-coating chlorite and good reservoir quality occurs in heterolithic distributary mouth bar sandstones, however mixing of mud- and sand-prone facies due to intense bioturbation has reduced permeability. Results from this study can be used to predict reservoir quality in the Smørbukk field and in analogous shallow-marine sandstones worldwide.

Item Type: Article
Uncontrolled Keywords: Chlorite, Grain-coating chlorite, Pore-filling chlorite, Deltaic sandstones, Reservoir quality, SEM-EDS, Porosity, Permeability
Divisions: Faculty of Science and Engineering > School of Environmental Sciences
Depositing User: Symplectic Admin
Date Deposited: 09 Sep 2021 10:07
Last Modified: 02 May 2023 10:53
DOI: 10.1016/j.marpetgeo.2021.105326
Related URLs:
URI: https://livrepository.liverpool.ac.uk/id/eprint/3136487