Skip to main content

7 Result(s)

within G. Manatschal Remove this filter

and

  1. No Access

    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)

  2. No Access

    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)

  3. No Access

    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)

  4. No Access

    Article

    The Sondalo gabbro contact aureole (Campo unit, Eastern Alps): implications for mid-crustal mafic magma emplacement

    Contact aureoles rimming plutonic rocks are the locus of metamorphism and deformations witnessing magma emplacement mechanisms in the crust. In this study, structural and petrological observations are combined...

    B. Petri, G. Mohn, P. Štípská, K. Schulmann… in Contributions to Mineralogy and Petrology (2016)

  5. No Access

    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)

  6. No Access

    Chapter

    Rifted Margins: Building Blocks of Later Collision

    Rifted margins develop by the splitting apart of continents and form the trailing edges of ocean basins, to be incorporated into collision zones when those basins eventually close. Magma-poor margins are domin...

    T. Reston, G. Manatschal in Arc-Continent Collision (2011)

  7. No Access

    Article

    Evolution of magma-poor continental margins from rifting to seafloor spreading

    The rifting of continents involves faulting (tectonism) and magmatism, which reflect the strain-rate and temperature dependent processes of solid–state deformation and decompression melting within the Earth1,2. M...

    R. B. Whitmarsh, G. Manatschal, T. A. Minshull in Nature (2001)