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Secondary porosity development in incised valley sandstones from two wells from the Flemish Pass area, offshore Newfoundland

In this study we discuss the diagenetic processes that have contributed to the preservation of anomalously high secondary porosity (20–30%) and associated high permeability in relative deeply buried (2–3 km) Tithonianaged stacked incised valley reservoir sandstone intervals (informally named Ti-2 and Ti-3) in the Flemish Pass area, offshore Newfoundland.

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Effect of sediment source on source rock hydrocarbon potential; An example from the Kimmeridgian and Tithonian-aged source rocks of the central ridge, off-shore Newfoundland, Canada

This study presents an integrated approach using organic geochemistry and incident-light organic petrographic microscopy techniques to characterize kerogen type, hydrocarbon potential, thermal maturity, and the effect depositional environment has on five wells from Upper-Jurassic Kimmeridgian and Tithonian-aged source rock intervals in the Central Ridge area offshore Newfoundland, Canada.

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Secondary porosity development in incised valley sandstones from two wells from the Flemish Pass area, offshore Newfoundland

In this study we discuss the diagenetic processes that have contributed to the preservation of anomalously high secondary porosity (20–30%) and associated high permeability in relative deeply buried (2–3 km) Tithonianaged stacked incised valley reservoir sandstone intervals (informally named Ti-2 and Ti-3) in the Flemish Pass area, offshore Newfoundland.

read more

Effect of sediment source on source rock hydrocarbon potential; An example from the Kimmeridgian and Tithonian-aged source rocks of the central ridge, off-shore Newfoundland, Canada

This study presents an integrated approach using organic geochemistry and incident-light organic petrographic microscopy techniques to characterize kerogen type, hydrocarbon potential, thermal maturity, and the effect depositional environment has on five wells from Upper-Jurassic Kimmeridgian and Tithonian-aged source rock intervals in the Central Ridge area offshore Newfoundland, Canada.

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