Radiocarbon chronology of the last glacial maximum and its termination in northwestern Patagonia
We examine the timing and magnitude of the last glacial maximum (LGM) and the last
glacial termination (LGT) in northwestern Patagonia, situated in the middle latitudes of South …
glacial termination (LGT) in northwestern Patagonia, situated in the middle latitudes of South …
[HTML][HTML] Synchronisation of sedimentary records using tephra: A postglacial tephrochronological model for the Chilean Lake District
Well-characterised tephra horizons deposited in various sedimentary environments provide
a means of synchronising sedimentary archives. The use of tephra as a chronological tool is …
a means of synchronising sedimentary archives. The use of tephra as a chronological tool is …
The evolution of the Onaping Formation at the Sudbury impact structure
RAF Grieve, DE Ames, JV Morgan… - Meteoritics & Planetary …, 2010 - Wiley Online Library
The 1.4–1.6 km thick Onaping Formation consists of a complex series of breccias and “melt
bodies” lying above the Sudbury Igneous Complex (SIC) at the Sudbury impact structure …
bodies” lying above the Sudbury Igneous Complex (SIC) at the Sudbury impact structure …
Contrasting records from mantle to surface of Holocene lavas of two nearby arc volcanic complexes: Caburgua-Huelemolle Small Eruptive Centers and Villarrica …
E Morgado, MA Parada, C Contreras… - Journal of Volcanology …, 2015 - Elsevier
Most of the small eruptive centers of the Andean Southern Volcanic Zone are built over the
Liquiñe-Ofqui Fault Zone (LOFZ), a NS strike-slip (> 1000 km length) major structure, and …
Liquiñe-Ofqui Fault Zone (LOFZ), a NS strike-slip (> 1000 km length) major structure, and …
The mafic Curacautín ignimbrite of Llaima volcano, Chile
Mafic volcanism accounts for 80% of magmas erupted on Earth. Although the majority of
these eruptions are effusive to Strombolian and fountain-fed, large explosive mafic eruptions …
these eruptions are effusive to Strombolian and fountain-fed, large explosive mafic eruptions …
Numerical modeling of time-dependent fluid dynamics and differentiation of a shallow basaltic magma chamber
F Gutiérrez, MA Parada - Journal of Petrology, 2010 - academic.oup.com
This contribution presents a numerical model of time-dependent physical processes and
differentiation in a cooling magma chamber to obtain the magma and liquid composition and …
differentiation in a cooling magma chamber to obtain the magma and liquid composition and …
Mineralogical and numerical approaches to establish the pre-eruptive conditions of the mafic Licán Ignimbrite, Villarrica Volcano (Chilean Southern Andes)
S Lohmar, M Parada, F Gutiérrez, C Robin… - Journal of Volcanology …, 2012 - Elsevier
The Licán Ignimbrite represents a large explosive basaltic andesite event in the eruptive
history of the Villarrica Volcano, an active stratovolcano of the Southern Andean Volcanic …
history of the Villarrica Volcano, an active stratovolcano of the Southern Andean Volcanic …
A late Holocene explosive mafic eruption of Villarrica volcano, Southern Andes: The Chaimilla deposit
L Costantini, L Pioli, C Bonadonna, J Clavero… - Journal of volcanology …, 2011 - Elsevier
Villarrica (Chile) is one of the most active volcanoes in South America having erupted about
60 times in the last 460years. Although its historical eruptive activity has been mainly …
60 times in the last 460years. Although its historical eruptive activity has been mainly …
Emplacement of unusual rhyolitic to basaltic ignimbrites during collapse of a basalt-dominated caldera: The Halarauður eruption, Krafla (Iceland)
Deposits of the ca. 110 ka Halarauður eruption of Krafla caldera (reconstructed volume= 7±6
km3 dense rock equivalent) include the only spatter-rich ignimbrite known in Iceland, and an …
km3 dense rock equivalent) include the only spatter-rich ignimbrite known in Iceland, and an …
Temporal magma source changes at Gaua volcano, Vanuatu island arc
A Beaumais, H Bertrand, G Chazot, L Dosso… - Journal of Volcanology …, 2016 - Elsevier
Abstract Gaua Island (also called Santa Maria), from the central part of the Vanuatu arc,
consists of a large volcano marked by a caldera that hosts the active Mount Garet summit …
consists of a large volcano marked by a caldera that hosts the active Mount Garet summit …