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Chaotic Mixing Device
09 May 2014 | Contributor(s):: Daniele Morgavi, Diego Perugini, Cristina P. De Campos, Werner Ertel-Ingrisch, Donald B. Dingwell
Description of device for chaotic mixing experiments developed at LMU München
Chiara Paola Montagna
Dimitrios P. Zouzias
Experimental constraints on magma mixing: case studies from Phlegrean Fields and Montserrat
30 Apr 2013 | Contributor(s):: Daniele Morgavi, Diego Perugini, Bettina Scheu, Cristina P. De Campos, Donald B. Dingwell
The mixing process in nature is observed at different scales in the rock record, evident through variable structural and textural patterns and morphologies such as filament-like structures, enclaves, and mineral phases showing physico-chemical disequilibrium. The type and geometry of these...
Magma mixing dynamics and associated geophysical signals
08 Oct 2015 | Contributor(s):: Chiara Paola Montagna, Antonella Longo, Paolo Papale, Matteo Bagagli
Primitive, volatile-rich magma arrival from depth into a degassed, evolved reservoir at 3km depth is investigated. The two magmatic end-member mix very efficiently on time scales of hours. The evolution is characterized by very heterogeneous pressure variations in space and time, showing...
Mixing- to-eruption timescales: an integrated model combining numerical simulations and high-temperature experiments with natural melts
12 Jun 2015 | Contributor(s):: Chiara Paola Montagna, Diego Perugini, Cristina De Campos, Antonella Longo, Donald B. Dingwell, Paolo Papale
Time scales of mingling in shallow reservoirs
14 Mar 2014 | Contributor(s):: Chiara Paola Montagna, Paolo Papale, Antonella Longo
Presentation at VUELCO meeting in Bristol, September 2013
Poster presentation at Goldschmidt 2013, Florence
Timescales of mingling in shallow magmatic reservoirs
12 Jun 2015 | Contributor(s):: Chiara Paola Montagna, paolo papale, antonella longo
Arrival of magma from depth into shallow reservoirs has been documented as one of thepossible processes leading to eruption. Magma intruding and rising to the surface interacts with thealready emplaced, degassed magmas residing at shallower depths, leaving chemical signatures inthe erupted...