AOGS-AGU (WPGM) Session: SE85 Time scales of magmatic evolution and eruption in intermediate to silicic magmatic system
From: Shan de Silva <desilvas@xxxxxxxxxxxxxxxxxxx>
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Dear Colleagues (apologies for multiple postings)
We
invite you to present your work on magmatic and eruption time scales
at the AOGS-AGU (WPGM) joint assembly in Singapore (13 -17, August
2012).
Abstract submission deadline is March 12.
More details on http://www.asiaoceania.org/aogs2012/index.asp
Session Title SE85 Time scales of magmatic evolution and eruption in intermediate to silicic magmatic system
Keynotes (invited): Simon Turner (Macquarie, Australia), Fidel Costa (EOS, Singapore)Convener(s)Prof. Shanaka de Silva (Oregon State University, United States), desilvas@xxxxxxxxxxxxxxxxxxx
Prof. Michihiko NAKAMURA (TOHOKU Univ., Japan), nakamm@xxxxxxxxxxxxxx
Dr. Phil SHANE (University of Auckland, New Zealand), pa.shane@xxxxxxxxxxxxxx
Session Description:The processes of magma generation, transport, storage, differentiation, and eruption control the timescales over which magmas evolve to eruption, as well as the nature of the resulting eruptions. Thus, linking processes and timescales of magma generation and evolution to eruptive behavior and eruptive volume is a fundamental goal for understanding and predicting the behavior of volcanic systems. This session will explore the range of time scales that characterize intermediate and silicic magma systems with particular reference to the Pacific Rim. Examples of themes include: [1] the relative roles and timescales of open versus closed system processes in the development of these magma systems [2] the time scales of assimilation and recharge events; [3] origin and residence times of the "crystal cargo" and the implications for the longevity of magmatic systems; [4] timescales of magma differentiation; [5] the link between eruptive volume and pre-eruptive magma residence timescales; [6] experimental constraints on eruptive processes and time scales; [7] link between physical properties and magmatic and eruptive time scales. The challenges of dealing with time-scales that may range from hundreds of thousands of years to hours requires a multidisciplinary, multi-scale effort and approaches that are field-based, multi-scale analytical, experimental, or numerical and analytical modeling from volcanonology, igneous petrology, geochemistry, geophysics, and experimental petrology and other relevant fields will be sought.
Professor
Departmentof Geosciences
Wilkinson Hall 104
Oregon State University
Corvallis
OR 97331
Ph: 541 737 1212
Fax: 541 737 1201
http://www.geo.oregonstate.edu/people/faculty/Shan_deSilva
http://www.geo.oregonstate.edu/research_groups/viper/main.htm
VolcanoWorld - http://volcano.oregonstate.edu
Increasing Diversity in the Earth Sciences
http://ides.science.oregonstate.edu
PLUTONS - exploring the Volcano-Plutonic Connection
http://plutons.science.oregonstate.edu
Departmentof Geosciences
Wilkinson Hall 104
Oregon State University
Corvallis
OR 97331
Ph: 541 737 1212
Fax: 541 737 1201
http://www.geo.oregonstate.edu/people/faculty/Shan_deSilva
http://www.geo.oregonstate.edu/research_groups/viper/main.htm
VolcanoWorld - http://volcano.oregonstate.edu
Increasing Diversity in the Earth Sciences
http://ides.science.oregonstate.edu
PLUTONS - exploring the Volcano-Plutonic Connection
http://plutons.science.oregonstate.edu
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