The birth of a new monogenetic volcano is difficult to forecast with precision, both in space and time. Nevertheless, seismic activity can alert of the imminence of such an eruption …
The Zacapu lacustrine basin is located in the north-central part of the Michoacán- Guanajuato volcanic field (MGVF), which constitutes the west-central segment of the Trans …
Abstract El Astillero and El Pedregal monogenetic volcanoes formed∼ 500–700 CE in the Tancítaro region in the southern part of the Michoacán-Guanajuato volcanic field, only 25 km …
The Michoacán–Guanajuato volcanic field (MGVF) in the western Trans-Mexican Volcanic Belt is one of the largest and most diverse monogenetic volcanic fields in the world holding …
Monogenetic volcanic fields occur in many tectonic settings representing an unpredictable and uncertain volcanic hazard. The Pátzcuaro Lake is located in the central part of the …
Four monogenetic Holocene lava flows located within the Michoacán-Guanajuato Volcanic Field, Mexico, were sampled for paleomagnetic dating. These flows (namely, El Infiernillo …
The Michoacán–Guanajuato Volcanic Field is the largest subduction-related monogenetic volcanic field in the world and includes more than 1000 scoria cones and a few hundred …
P Kshirsagar, C Siebe, MN Guilbaud… - Journal of Volcanology and …, 2016 - Elsevier
Abstract The 28,300 year BP (cal 32,300 BP) El Caracol tuff cone complex is one of the few phreatomagmatic volcanoes in the scoria-cone dominated Plio-Quaternary Michoacán …
Emplacement dynamics of highly viscous, silicic lava flows remain poorly constrained due to a lack of consideration of crystal-rich cases. Emplacement models mostly apply to glassy or …