Massif Central (France): new constraints on the geodynamical evolution from teleseismic tomography |
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| Authors: | M Granet G Stoll J Dorel U Achauer G Poupinet K Fuchs |
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| Institution: | École et Observatoire de Physique du Globe, 5 rue RenéDescartes, F-67084 Strasbourg Cédex, France;Geophysikalisches Institut, Hertzstrasse 16, D-76187 Karlsruhe, Germany;Observatoire de Physique du Globe, 12 avenue des Landais, F-63000 Clermont-Ferrand, France;Laboratoire de Géophysique Interne et Tectonophysique, BP 53 X, F-38041 Grenoble Cédex, France |
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| Abstract: | The Massif Central, the most significant geomorphological unit of the Hercynian belt in France, is characterized by graben structures which are part of the European Cenozoic Rift System (ECRIS) and also by distinct volcanic episodes, the most recent dated at 20 Ma to 4000 years BP. In order to study the lithosphere-asthenosphere system beneath this volcanic area, we performed a teleseismic field experiment.
During a six-month period, a joint French-German team operated a network of 79 mobile short-period seismic stations in addition to the 14 permanent stations. Inversion of P -wave traveltime residuals of teleseismic events recorded by this dense array yielded a detailed image of the 3-D velocity structure beneath the Massif Central down to 180 km depth. The upper 60 km of the lithosphere displays strong lateral heterogeneities and shows a remarkable correlation between the volcanic provinces and the negative velocity perturbations. The 3-D model reveals two channels of low velocities, interpreted as the remaining thermal signature of magma ascent following large lithospheric fractures inherited from Hercynian time and reactivated during Oligocene times. The teleseismic inversion model yields no indication of a low-velocity zone in the mantle associated with the graben structures proper. The observation of smaller velocity perturbations and a change in the shape of the velocity pattern in the 60–100 km depth range indicates a smooth transition from the lithosphere to the asthenosphere, thus giving an idea of the lithosphere thickness. A broad volume of low velocities having a diameter of about 200 km from 100 km depth to the bottom of the model is present beneath the Massif Central. This body is likely to be the source responsible for the volcanism. It could be interpreted as the top of a plume-type structure which is now in its cooling phase. |
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| Keywords: | 3-D inversion of P delays mantle plume-type structure Massif Central volcanic provinces |
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