Patricio H. Figueredo

TL;DR: In this article, the authors highlight the occurrence of two major decoupling horizons controlling the structural and magmatic evolution of distal magma-poor rifted margins and suggest that during final rifting the strain distribution is controlled first by hydration and then by magmatic processes in the domain of exhumed mantle.

TL;DR: In this paper, the Austroalpine and Upper Penninic nappes in the Central Alps were investigated to understand the overall spatial and temporal evolution and resulting sedimentary stacking patterns within an evolving hyper-extended rift system.

TL;DR: In this article, the authors investigate the sedimentary system located at their toe across magma-poor rifted margins and show that mega fault-scarps are preferentially located at rift domain boundaries, implying a topographic escarpment that juxtaposes rift domains of different crustal thickness.

TL;DR: In this paper, the authors investigated the hydrothermal fluid circulation that was linked to the extensional evolution of the Adriatic rifted margin during the Jurassic opening of the Alpine Tethys.

TL;DR: In this article, sedimentological, structural, and petrographical observations and detrital zircon provenance data were used to document the processes controlling continental hyperextension and mantle exhumation.