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- W1604489180 abstract "The Late Devonian/Early Carboniferous (Tournaisian) Horton Bluff Formation formed within the tectonically subsiding Windsor Subbasin with a major bounding fault (Cobequid Fault precursor) to the north and with onlapping relationships to the south. The formation is divided into four members, in ascending order the Harding Brook, Curry Brook, Blue Beach and Hurd Creek Members. The formation is at least 560 m thick in the type area (Avon River Valley), and has its greatest measured thickness (1,015 m) in the Soquip Noel #1 well." @default.
- W1604489180 created "2016-06-24" @default.
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- W1604489180 date "1990-01-01" @default.
- W1604489180 modified "2023-09-23" @default.
- W1604489180 title "Stratigraphy, fluviolacustrine sedimentology and cyclicity of the Late Devonian/Early Carboniferous Horton Bluff Formation, Nova Scotia, Canada." @default.
- W1604489180 hasPublicationYear "1990" @default.
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