Neoproterozoic to Cambrian isolation of Laurentia during the breakup of Rodinia was
associated with multiple large igneous provinces, protracted multiphase rifting, and variable …

Oceanic hotspots with extreme enriched mantle radiogenic isotopic signatures—including
low 143Nd/144Nd indicative of subducted continental crust—are linked to plume conduits …

The amalgamation of Laurentia's Archean provinces ca. 1830 Ma was followed by~ 700 my
of accretionary orogenesis along its active southeastern margin, marked by subduction of …

Abstract The late Neoproterozoic–Cambrian interval is characterized by global-scale
orogenesis, rapid continental growth and profound changes in Earth systems. Orogenic …

The Laramide foreland belt comprises a broad region of thick-skinned, contractional
deformation characterized by an anastomosing network of basement-cored arches and …

Al sureste de la Cordillera Real, en la sección del río Miriumi, rocas sedimentarias e ígneas
metamorfoseadas fueron agrupadas sin discriminación en la Unidad Upano, y la falla …

The Rodinia supercontinent broke apart during the Neoproterozoic. Rodinia break-up is
associated with widespread intraplate magmatism on many cratons, including the c. 720 …

Abstract The Choquequirao Formation is a> 3 km-thick amphibolite-grade succession that
outcrops in the Central Andes of southern Peru. To constrain its age and tectonostratigraphic …

Changes in lithospheric composition and strength associated with rifting of the Rodinian
supercontinent (ca. 780− 485 Ma) served to localize Mesozoic tectonic activity in the McCall …

Highlights•The Arequipa rift back-arc basin controlled by three major graben-bounding fault
systems.•They were the favourable places for tectonic inversion, shortening, thickening and …