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AGU Fall Meeting 2013: GP011 Magnetic studies of igneous processes
From: Michael Ort <Michael.Ort@xxxxxxx>
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We would like to invite you to submit an abstract to the AGU Fall Meeting session described below.
GP011 Magnetic studies of igneous processes
Paleomagnetic, rock magnetic, and magnetic anomaly data can be used to constrain a variety of igneous or volcanic processes. Common applications include using paleosecular variation to constrain eruptive timing; blocking temperatures to estimate emplacement temperatures; magnetic anisotropy to constrain flow direction; paleomagnetic data to constrain tilt and rotation; oxide mineralogy to infer a temperature-oxidation path; or magnetic anomaly data to infer subsurface size/shape or extent of hydrothermal alteration. We solicit any applied studies using paleomagnetic, rock magnetic or magnetic anomaly data to infer igneous process. We also especially welcome experimental, theoretical, or other contributions that explore the reliability and theoretical underpinning of these methods.
Conveners:
Julie Bowles University of Wisconsin - Milwaukee; bowlesj@xxxxxxx
John Geissman, University of Texas at Dallas, geissman@xxxxxxxxxxxx
Michael Ort, Northern Arizona University, michael.ort@xxxxxxx
Abstracts are due August 6. The meeting will take place in San Francisco 9-13 December, 2013.
Michael
Michael Ort
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AGU Fall Meeting 2013: GP011 Magnetic studies of igneous processes
From: Michael Ort <Michael.Ort@xxxxxxx>
************************************************************************************************
We would like to invite you to submit an abstract to the AGU Fall Meeting session described below.
GP011 Magnetic studies of igneous processes
Paleomagnetic, rock magnetic, and magnetic anomaly data can be used to constrain a variety of igneous or volcanic processes. Common applications include using paleosecular variation to constrain eruptive timing; blocking temperatures to estimate emplacement temperatures; magnetic anisotropy to constrain flow direction; paleomagnetic data to constrain tilt and rotation; oxide mineralogy to infer a temperature-oxidation path; or magnetic anomaly data to infer subsurface size/shape or extent of hydrothermal alteration. We solicit any applied studies using paleomagnetic, rock magnetic or magnetic anomaly data to infer igneous process. We also especially welcome experimental, theoretical, or other contributions that explore the reliability and theoretical underpinning of these methods.
Conveners:
Julie Bowles University of Wisconsin - Milwaukee; bowlesj@xxxxxxx
John Geissman, University of Texas at Dallas, geissman@xxxxxxxxxxxx
Michael Ort, Northern Arizona University, michael.ort@xxxxxxx
Abstracts are due August 6. The meeting will take place in San Francisco 9-13 December, 2013.
Michael
Michael Ort
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