Dolomitization of the Lower Ordovician Aguathuna Formation carbonates, Port au Port Peninsula, western Newfoundland, Canada: implications for a hydrocarbon reservoir
The Lower Ordovician Aguathuna Formation (∼100 m thick) is formed of shallow-marine carbonates, which constitute the uppermost part of the St. George Group of western Newfoundland. Sedimentation was paused by a major subaerial exposure (St. George Unconformity), which likely developed a significant...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
NRC Research Press
2008
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Subjects: | |
Online Access: | https://research.library.mun.ca/11723/ https://research.library.mun.ca/11723/1/Azmy_et_al_2008_b_CJES.pdf https://doi.org/10.1139/E08-020 |