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Diagenetic history of Ordovician and Devonian oil ... - Geology Ontario

Diagenetic history of Ordovician and Devonian oil ... - Geology Ontario

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STUDY AREA<br />

The study area is located in the extreme southwest corner <strong>of</strong> <strong>Ontario</strong> (Figure 2).<br />

<strong>Ordovician</strong> <strong>oil</strong> <strong>and</strong> gas pools are found throughout southern <strong>Ontario</strong>, but the majority <strong>of</strong><br />

currently producing pools are located here. Many <strong>of</strong> the earlier discovered pools, such as<br />

Hepworth <strong>and</strong> Acton, are no longer in production. From southwest to northeast the wells<br />

examined include those located in the following pools: Malden, Colchester, Hillman,<br />

Goldsmith-Wheatley, Renwick, Dover <strong>and</strong> Lambton. Each pool typically has one or two<br />

cores available with the exception <strong>of</strong> the Hillman pool which has four cores. In order to<br />

observe the pre-fracturing characteristics <strong>and</strong> compare pre- <strong>and</strong> post-fracturing diagenesis a<br />

core (OGS-82-2 Harwich 25-DECR in Kent County) located away from the <strong>oil</strong> pools was<br />

also examined.<br />

METHODOLOGY<br />

A list <strong>of</strong> the wells used in the study <strong>and</strong> core descriptions are presented in<br />

Appendix 1. Approximately 350 thin sections were produced <strong>and</strong> stained with potassium<br />

ferricyanide to indicate relative iron content <strong>and</strong> Alizaran Red-S to distinguish between<br />

calcite <strong>and</strong> dolomite. The microscopic examination includes transmitted light <strong>and</strong><br />

cathodoluminescence. Geochemical analyses include major <strong>and</strong> trace elements (Ca, Mg,<br />

Fe, Mn <strong>and</strong> Sr) <strong>of</strong> limestone <strong>and</strong> dolomite examined with microprobe <strong>and</strong> stable isotopes<br />

(C <strong>and</strong> O) <strong>of</strong> limestone <strong>and</strong> dolomite.<br />

Thirty-two samples <strong>of</strong> dolomite <strong>and</strong> sixteen <strong>of</strong> limestone were drilled with a<br />

modified dental drill for bulk analyses <strong>of</strong> stable carbon <strong>and</strong> oxygen isotopes. The analyses<br />

were performed at the University <strong>of</strong> Waterloo on a VGMM903 mass spectrometer.

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