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From: HEAP Michael <heap@xxxxxxxxxx>
Subject: EGU 2017: Fluids, Cracks, Pores & Permeability in Crustal, Magmatic and Volcanic Environments
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Dear Colleagues,
We would like to draw your attention to the session Fluids, Cracks, Pores & Permeability in Crustal, Magmatic and Volcanic Environments (GMPV4.3/EMRP4.30/TS3.8) at the EGU General Assembly in Vienna, Austria, 23 -28 April 2017.
We encourage contributions that integrate results from field, experimental, theoretical, and numerical and analytical modelling. The session is described below.
To submit an abstract please follow the link: http://meetingorganizer.copernicus.org/EGU2017/session/24713
Note that abstract submission deadline is 11 January 2017 13:00 CET and the deadline for support applications is 01 December 2016.
Looking forward to Vienna!
Best wishes,
The conveners
GMPV4.3/EMRP4.30/TS3.8
Convener: Jackie E. Kendrick; Co-Conveners: Michael Heap, Kelly Russell, and Caroline Martel
Permeability is a fundamental physical property which helps dictate geological processes across a range of time- and length-scales. For example, during volcanic activity (e.g., magma transport, eruption) permeability can be created and/ or destroyed, controlling the means and efficiency of outgassing and, thereby, affecting eruption style and intensity. In addition, permeability and permeability anisotropy of crustal rocks dictate fluid flow in the lithosphere, controlling crustal pore pressures and seismicity along shallow or deep lithospheric structures, as well as the productivity and exploitation of georesources. Technological advances facilitate ever-more detailed descriptions of permeability and yet critical challenges remain; for example, understanding the evolution (e.g., creation or destruction) of permeability, the extent of processes as a function of time/ strain/ stress and the influence of realistic geological conditions (including temperature, large and/ or fluc
tuating pressure gradients, destructive pore fluids etc.). Here, we invite field-, experimental-, technical-, theoretical- and model-based studies that discuss or tackle permeability development, constraint or evolution critical to many facets of geoscience. Our intent is to foster strong interactions between research groups by soliciting contributions from diverse subdisciplines including (but not limited to) volcanology, rock and magma mechanics and physics, petrology, structural geology, and geophysics. We particularly welcome abstracts from early career scientists.
--
Mike HEAP
Maître de conférences
Personal website: http://eost.unistra.fr/recherche/ipgs/ge/ge-perso/michael-heap/
Lab website: http://eost.unistra.fr/recherche/ipgs/ge/ge-perso/michael-heap/laboratoire-de-deformation-des-roches/
Laboratoire de Déformation des Roches
Équipe de Géophysique Expérimentale
Institut de Physique de Globe de Strasbourg
UMR 7516 CNRS, Université de Strasbourg/EOST
5 rue René Descartes
67084 Strasbourg cedex
FRANCE
We would like to draw your attention to the session Fluids, Cracks, Pores & Permeability in Crustal, Magmatic and Volcanic Environments (GMPV4.3/EMRP4.30/TS3.8) at the EGU General Assembly in Vienna, Austria, 23 -28 April 2017.
We encourage contributions that integrate results from field, experimental, theoretical, and numerical and analytical modelling. The session is described below.
To submit an abstract please follow the link: http://meetingorganizer.
Note that abstract submission deadline is 11 January 2017 13:00 CET and the deadline for support applications is 01 December 2016.
Looking forward to Vienna!
Best wishes,
The conveners
GMPV4.3/EMRP4.30/TS3.8
Convener: Jackie E. Kendrick; Co-Conveners: Michael Heap, Kelly Russell, and Caroline Martel
Permeability is a fundamental physical property which helps dictate geological processes across a range of time- and length-scales. For example, during volcanic activity (e.g., magma transport, eruption) permeability can be created and/ or destroyed, controlling the means and efficiency of outgassing and, thereby, affecting eruption style and intensity. In addition, permeability and permeability anisotropy of crustal rocks dictate fluid flow in the lithosphere, controlling crustal pore pressures and seismicity along shallow or deep lithospheric structures, as well as the productivity and exploitation of georesources. Technological advances facilitate ever-more detailed descriptions of permeability and yet critical challenges remain; for example, understanding the evolution (e.g., creation or destruction) of permeability, the extent of processes as a function of time/ strain/ stress and the influence of realistic geological conditions (including temperature, large and/ or fluc
tuating pressure gradients, destructive pore fluids etc.). Here, we invite field-, experimental-, technical-, theoretical- and model-based studies that discuss or tackle permeability development, constraint or evolution critical to many facets of geoscience. Our intent is to foster strong interactions between research groups by soliciting contributions from diverse subdisciplines including (but not limited to) volcanology, rock and magma mechanics and physics, petrology, structural geology, and geophysics. We particularly welcome abstracts from early career scientists.
--
Mike HEAP
Maître de conférences
Personal website: http://eost.unistra.
Lab website: http://eost.unistra.
Laboratoire de Déformation des Roches
Équipe de Géophysique Expérimentale
Institut de Physique de Globe de Strasbourg
UMR 7516 CNRS, Université de Strasbourg/EOST
5 rue René Descartes
67084 Strasbourg cedex
FRANCE
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