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    Article

    Characteristics and timing of hydrothermal fluid circulation in the fossil Pyrenean hyperextended rift system: new constraints from the Chaînons Béarnais (W Pyrenees)

    The evolution of hyperextended rift systems is linked to complex tectonic processes in which fluid activity is much more important than previously thought. This study sheds light on the fluid-sediment interact...

    N. Incerpi, G. Manatschal, L. Martire in International Journal of Earth Sciences (2020)

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    Article

    Polyphase tectono-magmatic evolution during mantle exhumation in an ultra-distal, magma-poor rift domain: example of the fossil Platta ophiolite, SE Switzerland

    Despite the fact that many studies have investigated mantle exhumation at ultra-slow-spreading ridges and magma-poor rifted margins, there are still numerous questions concerning the 3D architecture, magmatic,...

    M.-E. Epin, G. Manatschal, M. Amman, C. Ribes in International Journal of Earth Sciences (2019)

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    Article

    U–Pb geochronology of the Sondalo gabbroic complex (Central Alps) and its position within the Permian post-Variscan extension

    The end of an orogenic cycle is commonly associated with a general extensional regime, widespread magmatism and complex metamorphic overprints. The Austroalpine domain in SE Switzerland and N Italy preserves a...

    B. Petri, G. Mohn, E. Skrzypek, T. Mateeva in International Journal of Earth Sciences (2017)

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    Article

    Rift-related inheritance in orogens: a case study from the Austroalpine nappes in Central Alps (SE-Switzerland and N-Italy)

    The Austroalpine nappe systems in SE-Switzerland and N-Italy preserve remnants of the Adriatic rifted margin. Based on new maps and cross-sections, we suggest that the complex structure of the Campo, Grosina/L...

    G. Mohn, G. Manatschal, E. Masini, O. Müntener in International Journal of Earth Sciences (2011)