The role of serpentinization and magmatism in the formation of decoupling interfaces at magma-poor rifted margins
In spite of recent progress in the understanding of magma-poor rifted margins, the processes
leading to the formation and evolution of the exhumed mantle domain and its transition …
leading to the formation and evolution of the exhumed mantle domain and its transition …
[HTML][HTML] Rifted margins classification and forcing parameters
F Sapin, JC Ringenbach, C Clerc - Scientific Reports, 2021 - nature.com
Rifted margins are the result of the successful process of thinning and breakup of the
continental lithosphere leading to the formation of new oceanic lithosphere. Observations on …
continental lithosphere leading to the formation of new oceanic lithosphere. Observations on …
Kinematic evolution of the southern North Atlantic: Implications for the formation of hyperextended rift systems
We focus on the southern North Atlantic rifted margins to investigate the partitioning and
propagation of deformation in hyperextended rift systems using plate kinematic modeling …
propagation of deformation in hyperextended rift systems using plate kinematic modeling …
Polyphase tectono-magmatic evolution during mantle exhumation in an ultra-distal, magma-poor rift domain: example of the fossil Platta ophiolite, SE Switzerland
ME Epin, G Manatschal, M Amman, C Ribes… - International Journal of …, 2019 - Springer
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 …
spreading ridges and magma-poor rifted margins, there are still numerous questions …
The syn‐rift tectono‐stratigraphic record of rifted margins (Part II): A new model to break through the proximal/distal interpretation frontier
One fundamental lesson from the last decade's research into rifted margins is that
stratigraphic horizons cannot be simply correlated from the proximal into distal domain …
stratigraphic horizons cannot be simply correlated from the proximal into distal domain …
The syn‐rift tectono‐stratigraphic record of rifted margins (Part I): Insights from the Alpine Tethys
The tectono‐stratigraphic evolution of rift systems is at present poorly understood, especially
the one preceding the onset of oceanic seafloor spreading. Improving our understanding of …
the one preceding the onset of oceanic seafloor spreading. Improving our understanding of …
Constraints imposed by rift inheritance on the compressional reactivation of a hyperextended margin: Mapping rift domains in the North Iberian margin and in the …
Abstract The Alpine Pyrenean‐Cantabrian orogen developed along the plate boundary
between Iberia and Europe, involving the inversion of Mesozoic hyperextended basins …
between Iberia and Europe, involving the inversion of Mesozoic hyperextended basins …
[HTML][HTML] Birth of an oceanic spreading center at a magma-poor rift system
Oceanic crust is continuously created at mid-oceanic ridges and seafloor spreading
represents one of the main processes of plate tectonics. However, if oceanic crust …
represents one of the main processes of plate tectonics. However, if oceanic crust …
Crustal architecture and evolution of the southwestern South China Sea: Implications to continental breakup
SP Chang, M Pubellier, M Delescluse, Y Qiu… - Marine and Petroleum …, 2022 - Elsevier
Abstract The South China Sea (SCS) is a marginal basin characterized by propagating
breakup and subsequent seafloor spreading during the Cenozoic. Our study investigates the …
breakup and subsequent seafloor spreading during the Cenozoic. Our study investigates the …
Thermal evolution of asymmetric hyperextended magma‐poor rift systems: Results from numerical modeling and Pyrenean field observations
We investigate the thermal and structural evolution of asymmetric rifted margin using
numerical modeling and geological observations derived from the Western Pyrenees. Our …
numerical modeling and geological observations derived from the Western Pyrenees. Our …