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Fig. 8 | Swiss Journal of Geosciences

Fig. 8

From: The Theodul Glacier Unit, a slab of pre-Alpine rocks in the Alpine meta-ophiolite of Zermatt-Saas, Western Alps

Fig. 8

Concordia diagram. Ellipses around individual data points indicate 2σ uncertainty. Upper intercept age of 295 ± 16 Ma is interpreted to reflect granulite facies metamorphism. The significance of the lower intercept is more uncertain; it is possible that isotopic resetting could have been caused by the processes related to Jurassic hyperextension, with further disturbances during the Alpine events

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