Reconstruction of proportions between juvenile and recycled crust remains challengeable
because a big part of juvenile source magmatic rocks formed at intra-oceanic arcs, can be …

Deep-sea fan sediments carry physical and chemical signatures that reflect the conditions
under which their native landscapes evolved. Fans are long-lived, strongly net-depositional …

Abstract The Great Valley basin of California (USA) is an archetypal forearc basin, yet the
timing, structural style, and location of basin development remain controversial. Eighteen of …

Abstract The SW Ecuador‐NW Peru forearc region is the southernmost location, where the
Caribbean large igneous province (CLIP) interacted with the South American margin since …

Ocean-continental subduction zones are commonly associated with compressional stress
fields, which ultimately result in regional uplift of the overriding plate. This has particularly …

A comparison of detrital zircon ages from the Cenozoic forearc basins in SW Ecuador–NW
Peru and those derived from the Amotapes Massif offers a singular opportunity to shed some …

The collision of oceanic arcs with continental margins is an important mechanism for the
growth of continents. Ancient forearc basin strata in collisional orogens provide a record of …

Detrital zircon U‐Pb and fission track double‐dating and Hf isotopes from the Mesozoic and
Cenozoic strata in the southern Alaska fore‐arc basin system reveal the effects of two …

The southwestern margin of Laurentia transitioned from a left-lateral transform margin to a
convergent margin by middle Permian time, which initiated the development of a subduction …

The link between plate tectonics and the evolution of active margins is still an ongoing task
to challenge since the acceptance of plate tectonic paradigm. This paper aims at …