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 …

Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur
in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas …

U–Pb geochronology along with elemental and Nd–Hf–Os isotopic data from the earliest
Neoproterozoic metabasic rocks within the Cathaysia Block of the South China Block (SCB) …

Abstract The Sangri Group volcanic rocks are distributed along the southern margin of the
Lhasa Terrane on the northern side of the Indus-Yarlung Zangbo suture zone. This Group …

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 …

The tectonic nature of the Cathaysia Block during earliest Neoproterozoic period has been
long disputed and attracted considerable attentions. One reason for this problem is rare …

Triassic volcanic rocks are mainly distributed in the central part of the San-Jiang orogenic
belt in southwestern China, and are exposed dominantly in the eastern segment of the …

Common geological, geochemical, and geophysical characteristics of continental fragments
of East Gondwana and adjacent oceanic lithosphere define a long‐lived, low‐volume …

Abstract The Middle America subduction zone (MASZ) is one of the world'most complex
convergent margins as it involves the subduction of the Rivera and Cocos young oceanic …