Single page posterPumice is a highly porous rock composed of volcanic glass bearing dense and complex networks of vesicles-- bubbles preserved in solid rock resulting from the exsolution of volatiles such as water and carbon dioxide from the magmatic melt during its ascent to the surface. These vesicles often become interconnected, rendering the magma permeable to buoyant gas which escapes into the host rock or the atmosphere. This process, which is known as outgassing, reduces the overpressure in the magma and may prevent fragmentation and explosive eruption. How permeability varies depends on the size, shape, and abundance of vesicles and fractures.The goal of my project is to analyze the physical properties of 3D printed pumice models. W...
Volcanic ash and pyroclasts can weld when deposited hot by pyroclastic density currents, in near-ven...
We have characterized the textures of pumice clasts from Phlegraean Fields to gain insights into the...
Plinian lapilli from the 1060 Common Era Glass Mountain rhyolitic eruption of Medicine Lake Volcano,...
Mafic eruptions, which are typically effusive to mildly explosive, can produce much stronger explosi...
This thesis consists of three projects based on magma ascent dynamics during volcanic eruptions. In ...
International audienceX-ray computed microtomography (μCT) was applied to pumices from the largest Q...
Effective models for the evolution of magma permeability are key to understanding shallow magma asce...
Understanding the influence of bubble foams on magma permeability and strength is critical to invest...
© Author(s) 2016. Understanding the physicochemical conditions extant and mechanisms operative durin...
Volcanic eruptions are driven by magma buoyancy caused by volatiles exsolving to form a separate gas...
Co-auteur étrangerInternational audiencePore connectivity is a measure of the fraction of pore space...
Volcanic ash and pyroclasts can weld when deposited hot by pyroclastic density currents, in near-ven...
We have characterized the textures of pumice clasts from Phlegraean Fields to gain insights into the...
Plinian lapilli from the 1060 Common Era Glass Mountain rhyolitic eruption of Medicine Lake Volcano,...
Mafic eruptions, which are typically effusive to mildly explosive, can produce much stronger explosi...
This thesis consists of three projects based on magma ascent dynamics during volcanic eruptions. In ...
International audienceX-ray computed microtomography (μCT) was applied to pumices from the largest Q...
Effective models for the evolution of magma permeability are key to understanding shallow magma asce...
Understanding the influence of bubble foams on magma permeability and strength is critical to invest...
© Author(s) 2016. Understanding the physicochemical conditions extant and mechanisms operative durin...
Volcanic eruptions are driven by magma buoyancy caused by volatiles exsolving to form a separate gas...
Co-auteur étrangerInternational audiencePore connectivity is a measure of the fraction of pore space...
Volcanic ash and pyroclasts can weld when deposited hot by pyroclastic density currents, in near-ven...
We have characterized the textures of pumice clasts from Phlegraean Fields to gain insights into the...
Plinian lapilli from the 1060 Common Era Glass Mountain rhyolitic eruption of Medicine Lake Volcano,...