Columnar-jointed bentonite below a Doleritic Sill, Tideswell Dale, Derbyshire, UK: formation during prograde contact metamorphism

Columnar-jointed tuffs (bentonites) are located below the Lower Carboniferous Tideswell Dale Sill, Derbyshire, in an abandoned quarry. There are three zones of prismatic joints, columnar joints (∼60 cm thick and mean column width of 4.1 cm) and massive, conchoidally fractured rock sequentially from...

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Veröffentlicht in:Geological magazine 2020-07, Vol.157 (7), p.1181-1198
Hauptverfasser: Mullineux, S, Sparks, RSJ, Murphy, MD, MacNiocaill, C, Barfod, D, Njorka, J, Schumacher, JC
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Sprache:eng
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