Neotethyan suprasubduction zone ophiolites represent anomalous oceanic crust developed
in older host basins during trench rollback cycles and later entrapped in orogenic belts as a …

Reconfigurations of magmatic arcs through time have been recognized since pioneering
works, describing inland and trenchward arc migrations or magmatic shut-off lasting for …

Suprasubduction zone (SSZ) ophiolites in orogenic belts represent oceanic crust generation
in subduction rollback cycles during the closing stages of basins prior to terminal continental …

The analyses of the main parameters controlling the present Chile‐type and Marianas‐type
tectonic settings developed along the eastern Pacific region show four different tectonic …

Modern-style plate tectonics can be tracked into the geologic past with petrotectonic
assemblages and other plate-tectonic indicators. These indicators suggest that modern plate …

Andesite magmatism at convergent margins is essential for the differentiation of silicate
Earth, but no consensus exists as to andesite petrogenesis. Models proposing origin of …

We report here a Cambrian southward-subducting intra-oceanic arc system in the southern
West Junggar, NW China, where an immature arc occurred initially on SSZ-type ophiolites …

Understanding the geological history of the Lhasa Terrane prior to the India–Asia collision (~
55±10 Ma) is essential for improved models of syn-collisional and post-collisional processes …

The customary practice for displaying REE abundances is to normalize them to chondritic
abundances and then to plot these normalized abundances in order of atomic number, Z …

Mantle flow is a key feature that can affect melt production and composition in and around
subduction zones. In this study, I use three-dimensional numerical models to investigate the …