V Basch, A Sanfilippo, SG Skolotnev… - Journal of …, 2022 - academic.oup.com
Abstract The Doldrums Megatransform System (~ 7–8° N, Mid-Atlantic Ridge) shows a complex architecture including four intra-transform ridge segments bounded by five active …
The exposure of gabbroic sequences at Oceanic Core Complexes (OCC) along ultraslow-to slow-spreading ridges permits the study of the processes forming the lower oceanic crust …
CT Onken, J Eberhard-Schmid, L Hauser, S Marioni… - Lithos, 2024 - Elsevier
Abstract The Venda Nova and Várzea Alegre Plutons in southeastern Brazil are post- collisional complexes formed during the gravitational collapse of the Araçuaí-Ribeira …
Despite the recent progress in seismic imaging and dynamic modelling, the tectono- magmatic evolution during late orogenic extension and rifting is at present little understood …
The Nidar ophiolite is one of the well-preserved and almost complete ophiolite sections of the Neo-Tethyan oceanic lithosphere, obducted along the continental margin between the …
The Jurassic ophiolites in the Northern Apennines and the Western Alps represent fossil mid- ocean ridge (MOR) oceanic lithosphere that formed in the Mesozoic Ligurian-Piedmont …
Many recent studies have investigated the replacive formation of troctolites from mantle protoliths and the compositional evolution of the percolating melt during melt–rock …
Deep melt intrusion and melt-peridotite interaction may introduce small-scale heterogeneity in the MORB mantle. These processes generate pyroxenite-bearing veined mantle that …
E Rampone, A Sanfilippo - Elements: An International …, 2021 - pubs.geoscienceworld.org
The Alpine–Apennine ophiolites are lithospheric remnants of the Jurassic Alpine Tethys Ocean. They predominantly consist of exhumed mantle peridotites with lesser gabbroic and …