The Mauléon basin is a world‐class example of hyperextended rift suture. The basin possesses key attributes of an optimal hydrogen target, namely mantle, at shallow depth …
Independent models of P wave and S wave velocity anomalies in the mantle derived from seismic tomography help to distinguish thermal signatures from those of partial melt …
The thick post-rift series that covers the Triassic to Lower Cretaceous sedimentary succession of the Lusitanian Basin, in west central Portugal, is crucial to understanding the …
The Alpine orogeny is well recorded onshore and offshore by tectonic inversion of the Mesozoic rift basins. Large scale linear seamounts (more than 250 km long and with up to 5 …
The combined effects of post‐rift magma emplacement and tectonic inversion on the hyper‐ extended West Iberian Margin are unravelled in detail using multichannel 2D/3D seismic …
Salt diapirism is a distinctive feature of the Mesozoic–Cenozoic basins of western Iberia and has been associated with petroleum seeps and shows since the dawn of petroleum …
The present structure of the Iberia–Africa plate boundary between the Gorringe Bank and the Algerian Basin is characterized by a highly segmented geometry and diffused seismicity …
About half of the rifted margins purportedly formed by extension with minor magmatism. The conceptual models of those magma-poor systems are greatly influenced by the continent-to …
Magma‐poor rifted margins can be affected by magmatic occurrences coeval with rifting and post‐rifting. Understanding the geological processes that originated these magmatic events …