Asymptotic quantization : based on 1984 Naples lectures by Abhay Ashtekar

By Abhay Ashtekar

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Identification of Deicke and Millbrig based on phenocryst mineralogy (Haynes, 1994). Abbreviation: sandstone, Ss. western Georgia and eastern Tennessee but occurs more consistently in the Bays Formation from northeastern Tennessee to near Daleville in western Virginia (Haynes, 1994). Southwestern Virginia and eastern Tennessee Correlating K-bentonites within southwestern Virginia and eastern Tennessee is a challenge because of the structural and stratigraphic complexities in this part of the Valley and Ridge province.

Abbreviation: sandstone, Ss. western Georgia and eastern Tennessee but occurs more consistently in the Bays Formation from northeastern Tennessee to near Daleville in western Virginia (Haynes, 1994). Southwestern Virginia and eastern Tennessee Correlating K-bentonites within southwestern Virginia and eastern Tennessee is a challenge because of the structural and stratigraphic complexities in this part of the Valley and Ridge province. Generally, the Middle and Upper Ordovician rocks are characterized by significant along-strike facies changes making it difficult to determine the continuity of rock units and their age relations.

Figure 55. Gull River Formation exposed near Coldwater, Ontario (locality 75). Base of hammer marks position of thin K-bentonite bed. Ordovician K-bentonites, eastern North America 75) and in a roadcut along Provincial Highway 7 on the west side of Marmora (locality 76). The Bobcaygeon Formation contains a K-bentonite at the base of the “Middle Member (Unit D)” about 6 m above the base of the formation. The bed is referred to as MR (Liberty, 1969). Diagnostic conodonts in the Bobcaygeon succession include P.

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