| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445189 | Journal of Structural Geology | 2011 | 18 Pages |
Abstract
⺠Anisotropy of magnetic susceptibility (AMS); 2D Gravity modelling; Extensional; deformation; pluton-dyke relationships; Variscan belt; Armorican Massif. ⺠The Carnac granitic complex is formed by the coalescence of NNE-SSW striking dykes. ⺠The internal granitic fabric is consistent with the WNW-ESE regional stretching. ⺠Its emplacement times the inception of the late-orogenic extensional deformation.
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Authors
P. Turrillot, M. Faure, G. Martelet, Y. Chen, R. Augier,