VOLCANO: AGU Session V15: Layered Intrusions

[Date Prev][Date Next][Thread Prev][Thread Next][Date Index][Thread Index]

 




******************************************************************************************************
AGU Session V15: Layered Intrusions
From: Madeleine Humphreys mcsh2@xxxxxxxxx
******************************************************************************************************

Dear all,

We would like to draw your attention to the following special session at the AGU Fall Meeting in December. We welcome and encourage submissions that address processes involved in the development of layered intrusions in the wider sense. The deadline for abstracts is *3rd September 2009*.

Fall AGU session: V15: Layered Intrusions

Sponsor: Volcanology, Geochemistry and Petrology

Convenors:

Madeleine C S Humphreys
Department of Earth Sciences, University of Cambridge
Downing Street
Cambridge, GBR  CB2 3EQ
+44 (0)1223 333400
mcsh2@xxxxxxxxx

Christian Tegner
Department of Earth Sciences, University of Aarhus
Høegh-Guldbergs Gade 2
Aarhus, DNK  DK-8000
+45 894 29456
christian.tegner@xxxxxxxxx

Marian B Holness
Department of Earth Sciences, University of Cambridge
Downing Street
Cambridge, GBR  CB2 3EQ
+44 (0)1223 333400
marian@xxxxxxxxxxxxx

Charles E Lesher
Department of Geology, UC Davis
One Shields Avenue
Davis, CA, USA  95616
(530) 752 9779
lesher@xxxxxxxxxxxxxxxxxxx



Description:

Layered intrusions represent a fascinating and complex manifestation of magma crystallisation and differentiation. They represent a key link between magma source and surface eruption, and can have significant economic impact through the development of mineral deposits. The study of layered intrusions brings together field geology, numerical and analogue modelling, fluid dynamics, experimental petrology and geochemical and textural study. Recent experimental, textural and geochemical work has highlighted the need for an integrated approach in order to constrain the underlying processes that control solidification, melt migration and efficiency of differentiation in mafic magma chambers. We encourage contributions that seek to advance our understanding of processes that control the development of layered intrusions, through integrated studies from any specialism.

============================================================== To unsubscribe from the volcano list, send the message: signoff volcano to: listserv@xxxxxxx, or write to: volcano-request@xxxxxxxx

To contribute to the volcano list, send your message to: volcano@xxxxxxxx Please do not send attachments. ==============================================================


[Index of Archives]     [Yosemite Backpacking]     [Earthquake Notices]     [USGS News]     [Yosemite Campgrounds]     [Steve's Art]     [Hot Springs Forum]

  Powered by Linux