Esquisse geologique de la peninsule Rallier du Baty, archipel de Kerguelen, terres australes et antarctiques francaises

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Abstract
The geologic structure of the Rallier du Baty peninsula (Kerguelen islands) is characterized by basaltic flows with an andesitic tendency, intruded by a volcano-pluton of quartziferous syenites which metamorphosed the basalt near its contacts. Recent superimposed acid volcanism is present, and fumarolic activity has been noted on the west coast.

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