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 …

Temporal changes in the chemical compositions of middle to late Miocene rocks from the
central Trans-Mexican Volcanic Belt elucidate how prolonged flat subduction influences arc …

Four species of spotted skunks (Carnivora, Mephitidae, Spilogale) are currently recognized:
Spilogale angustifrons, S. gracilis, S. putorius, and S. pygmaea. Understanding species …

Volcanoes switching from quiescence to eruption shortly after catastrophic earthquakes
have raised interest for volcanic triggering and the influence of earthquakes on volcanic …

Monogenetic volcanic fields have associated volcanic hazards that are not always well
constrained due to the lack of complete and well established geological and …

The voluminous succession of tholeiitic basalts, calc-alkaline andesites and minor high-K
basalts that form the Late Miocene Altos de Jalisco mafic province of the western Trans …

Volcán de Colima, one of the Earth's most active and hazardous andesitic stratovolcanoes,
experienced its last major explosive eruption on July 2015 with two distinct events. The July …

Abstract The Colima Volcanic Complex (CVC) is one of the most prominent volcanic edifices
within the Tran-Mexican Volcanic Belt (TMVB). Its evolution has been characterized by …

Sinters are siliceous rocks precipitated from geothermal waters typically formed in
continental volcanic provinces, where heat flux is significant and deep source fluids become …

The Querétaro region (central Mexico) is located in the trans‐Mexican volcanic belt, an
active volcanic arc related to the subduction of oceanic plates along the Pacific margin of …