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Batolito cornubiano

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Batolito Cornubiano

El Batolito cornubiano es una asociación de intrusiones de granito que yacen en la penínisula sud-occidental de la isla de Gran Bretaña, la cual es la parte del Reino Unido.. Las principales masas expuestas a la superficie del batolito se pueden observar en Dartmoor, Bodmin Moor, St Austell, Carnmenellis, Land's End y en las Islas Sorlingas. El batolito se formó a inicios del periodo geológico Pérmico de 300 a 275 millones a años atrás, en la fase tardía de la orogenia varisca.[1]​

Referencias

  1. ↑ Chen Y., Clark A.H., Farrar E., Wasteneys H.A.H.P., Hodgson M.J. & Bromley A.V. 1993. Diachronous and independent histories of plutonism and mineralization in the Cornubian Batholith, southwest England. Journal of the Geological Society, 150 pp. 1183–1191
Esta página se editó por última vez el 22 may 2021 a las 09:41.
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