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- W2344145867 abstract "A change from carbonates to various shales in eastern Canada occurred during Late Ordovician. In Middle to Late Ordovician there was formation of a tectonic foreland basin. Upper Ordovician black shales in eastern Canada include: Billings (eastern Ontario) Pointe Bleue (Lac St. Jean) Utica (southern Quebec) (50-300 m thick) Mccasty (Anticosti) The Utica Shale represents a sedimentological response to sea level high and restricted oceanic circulation. Maturation increases from oil in northeast lowlands to dry gas southwest of it. Since discovery in 2008, 30 Utica vertical horizontal wells have been drilled, with some good frac results. However, after a wide environmental assessment and definition of best practices, a 24-30-month de facto moratorium with limited activities went into effect." @default.
- W2344145867 created "2016-06-24" @default.
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- W2344145867 date "2011-01-01" @default.
- W2344145867 modified "2023-09-27" @default.
- W2344145867 title "The Upper Ordovician Utica and Lorraine Shales in Southern Quebec: A Regional Overview*" @default.
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