Hydrothermal eruptions are explosive events driven by the sudden and violent vaporization of the water present in many hot water geothermal fields worldwide. Over recent years, thermodynamical conditions of fluids and petrophisical-geomechanical features of host-rocks were mentioned as responsible of the wide range of eruptive styles and deposits of hydrothermal eruptions. Nevertheless, geological and historical records show that PDC and fallout processes are underestimated as common processes linked to hydrothermal eruptions. This paper analyzes from a multi-disciplinary approach —virtual outcrops modeling, sedimentology, petrographic and XDR studies, facies modeling, eye-witness source analysis, and stratigraphy— the pristine Holocene–his...
Detailed mapping of the Huaco intrusive Complex in NW Argentina documents a shift in the emplacement...
The Quaternary Campo de la Piedra Pomez ignimbrite (CPPI) is a superbly exposed, partially indurated...
The Cerro Munro sub-volcanic intrusion is emplaced in the back-arc (400 km from the trench) as small...
The Domuyo volcanic complex (Neuquén Province, Argentina) hosts one of the most promising geothermal...
Cerro Domuyo, in northwestern Neuquén province of Argentina, shows notable geothermal activity, alth...
The Pleistocene-Holocene Cerro Blanco Volcanic Complex (CBVC), one of the youngest caldera complexes...
Geothermal fields in subduction-related orogens are closely linked to areas characterized by young m...
Pyroclastic density currents (PDCs) are one of the most dangerous volcanic phenomena. The correct in...
The western slope of Cerro Domuyo in northern Patagonia is characterized by thermal springs with boi...
Laguna del Maule Volcanic Field (LdMVF, 36° 10′ S), located in the Southern Andean Volcanic Zone, co...
The crater lake and associated hydrothermal features of Copahue volcano have been studied intensivel...
This work describes the facies architecture, morphology and textures of a Jurassic rhyodacitic crypt...
Explosive volcanism in the Altiplano-Puna Volcanic Zone (APVZ) of the South American Central Andes f...
The Cerro Negro district, northwestern Deseado Massif (Patagonia, Argentina), is one of two world-cl...
The reconstruction of the stratigraphical-structural framework and the hydrogeology of geothermal ar...
Detailed mapping of the Huaco intrusive Complex in NW Argentina documents a shift in the emplacement...
The Quaternary Campo de la Piedra Pomez ignimbrite (CPPI) is a superbly exposed, partially indurated...
The Cerro Munro sub-volcanic intrusion is emplaced in the back-arc (400 km from the trench) as small...
The Domuyo volcanic complex (Neuquén Province, Argentina) hosts one of the most promising geothermal...
Cerro Domuyo, in northwestern Neuquén province of Argentina, shows notable geothermal activity, alth...
The Pleistocene-Holocene Cerro Blanco Volcanic Complex (CBVC), one of the youngest caldera complexes...
Geothermal fields in subduction-related orogens are closely linked to areas characterized by young m...
Pyroclastic density currents (PDCs) are one of the most dangerous volcanic phenomena. The correct in...
The western slope of Cerro Domuyo in northern Patagonia is characterized by thermal springs with boi...
Laguna del Maule Volcanic Field (LdMVF, 36° 10′ S), located in the Southern Andean Volcanic Zone, co...
The crater lake and associated hydrothermal features of Copahue volcano have been studied intensivel...
This work describes the facies architecture, morphology and textures of a Jurassic rhyodacitic crypt...
Explosive volcanism in the Altiplano-Puna Volcanic Zone (APVZ) of the South American Central Andes f...
The Cerro Negro district, northwestern Deseado Massif (Patagonia, Argentina), is one of two world-cl...
The reconstruction of the stratigraphical-structural framework and the hydrogeology of geothermal ar...
Detailed mapping of the Huaco intrusive Complex in NW Argentina documents a shift in the emplacement...
The Quaternary Campo de la Piedra Pomez ignimbrite (CPPI) is a superbly exposed, partially indurated...
The Cerro Munro sub-volcanic intrusion is emplaced in the back-arc (400 km from the trench) as small...