The Trans-Mexican Volcanic Belt (TMVB) is a 1000km long Neogene continental arc
showing a large variation in composition and volcanic style, and an intra-arc extensional …

Both Cretaceous arc-type and intraplate rocks are widely distributed in SE China, in
association with subduction of the paleo-Pacific Plate. However, it remains unclear whether …

Northeast China and adjacent regions are located in the central East Asian continent and
consist tectonically of both the Paleo-Asian and Paleo-Pacific orogens between the Siberian …

Seismic tomography studies and plate reconstructions suggest that the Farallon slab broke
off shortly before subduction ended off southern Baja California. However, the progress of …

La extraordinaria diversidad magmática de la Faja Volcánica Transmexicana está
controlada (directa o indirectamente) por dos placas oceánicas independientes cuyos …

The magmatic diversity of the Trans-Mexican Volcanic Belt is directly or indirectly controlled
by two independent oceanic plates with differing geophysical and compositional …

Abstract The Central Asian Orogenic Belt (CAOB, also known as the Altaid Tectonic
Collage), one of the largest and long-lived accretionary orogens in the world, developed …

Constraining the origin of the adakite–high-Nb basalt (HNB) association in Baja California,
Mexico, is critical to a better understanding of global arc magmatism. Currently the preferred …

The tectonic history and time of closure of the Palaeo-Asian ocean of the Altaids are issues
of lively current debate. To address these issues, this paper presents detailed geological …

Abstract The Devonian and Carboniferous rock assemblages in Western Junggar, southern
Altaids, include ophiolitic mélanges and coherent units. At Baijiantan, Yeyagou and Dagun …