The geochemistry of the volcanic rocks o
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T. E. Smith; P. E. Holm; M. F. Thirlwall
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Article
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2008
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John Wiley and Sons
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English
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## Abstract In late Oligocene or early Miocene, a series of basalts and basaltic andesites erupted on the island of Canouan and formed the Old Volcanic Massif (OVM). In a second eruptive phase a series of basalts, basaltic andesites and andesites formed the upper part of the Canouan Formation (CF;