Browsing by Subject "QE471.15.S25"

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Chlorite diagenesis in reservoir sandstones of the Lower Missisauga formation, offshore Nova Scotia

Gould, Kathleen (Halifax, N.S. : Saint Mary's University, 2007)

Diagenetic chlorite rims on quartz grains preserve porosity by preventing the formation of secondary, pore-filling quartz overgrowths in wells from the Venture and Thebaud fields. Elsewhere, in the Norwegian Sea and the ...
The relationship of trangressive systems tracts to sea-floor diagenesis, Lower Cretaceous, Scotian Basin

Okwese, Ann Chioma (Halifax, N.S. : Saint Mary's University, 2010)

The Lower Cretaceous rocks of the Scotian Basin are deltaic, with cycles of delta progradation with relatively high sedimentation rates, capped by a transgressive unit with lower sedimentation rates. The diagenetic mineral ...

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