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.
Hydrogen Index (HI) and Oxygen Index (OI) are two critical parameters for assessing the hydrocarbon potential and depositional environment of any source rocks.
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.
A detailed petrographic analysis was conducted on several core samples from the Cretaceous-aged Bluesky Formation in the La Glace area in Alberta, Canada.
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.
Hydrogen Index (HI) and Oxygen Index (OI) are two critical parameters for assessing the hydrocarbon potential and depositional environment of any source rocks.
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.
A detailed petrographic analysis was conducted on several core samples from the Cretaceous-aged Bluesky Formation in the La Glace area in Alberta, Canada.
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