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Geological Society, London, Special Publications; 2006; v. 253; p. 213-231;
DOI: 10.1144/GSL.SP.2006.253.01.11
© 2006 Geological Society of London

Models of Sedimentary Basins

Rifting through a heterogeneous crust: insights from analogue models and application to the Gulf of Corinth

L. Mattioni1,*, L. Le Pourhiet1,2 & I. Moretti1

1 Institut Français du Pétrole, Rueil Malmaison, France
2 Laboratoire de Tectonique, Université Pierre et Marie Curie, Paris, France
* Beicip Franlab, Rueil Malmaison, France luca.mattioni{at}beicip.fr

We used analogue models to study the fault evolution produced by extension through a heterogeneous crust. In the experiments, the heterogeneous crust consisted of a gently dipping silicone layer surrounded by brittle material. The viscous silicone level simulates a weak, upper crustal nappe stack that formed during a previous phase of shortening. X-ray scanner facilities allowed us to acquire 3D images of the experimental models at regular time invervals and hence to study the fault pattern development and the location of the main depocenters during rifting. The experimental results show that the inherited weak nappe stack acts as a décollement and localizes deformation. In the early stages of extension a system of conjugate high-angle normal faults initiates close to the upper tip of the gently dipping silicone layer near the free surface and propagates upwards, resulting in an initial symmetrical graben configuration. Further extension results in (1) a progressive asymmetry of the rifted zone, due to migration of its right margin down the nappe, (2) a shift of the main depocentre downward along the décollement, and (3) the simultaneous activity of several normal faults within the rifted zone. When the pre-existing silicone layer is oblique to the extension, the normal faults develop in an en echelon array, with a strike intermediate between the azimuth of the gently dipping silicone layer and the extension direction. The experiments also show how rheological differences between areas with potential intracrustal weak layers and adjacent domains without décollement level can lead to significant differences in fault pattern, dimension and orientation of the rifted zone. Complete asymmetry of a rift and switches in fault dip direction between adjacent domains can be explained by the presence of pre-existing upper crustal heterogeneities.