James Palandri
University of Oregon, Eugene, OR
Activity
2009
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A HYDROTHERMAL LIQUID LINE OF DESCENT FROM MAGMA TO EPITHERMAL FLUID
T239 Fluid-Driven Geochemical Transformations: In Honor of Harold HelgesonWednesday, 21 October 20098:00 AM - 12:00 PMPortland Ballroom 252
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STABLE-ISOTOPE AND PALEOSOL DATA FROM THE PLIO-PLEISTOCENE FISH CREEK-VALLECITO BASIN, SOUTHERN CALIFORNIA: NEW INSIGHTS INTO REGIONAL TECTONICS AND PALEOCLIMATE
222 Recent Advances in Paleoceanography and PaleoclimatologyWednesday, 21 October 20098:00 AM - 12:00 PMPortland Ballrooms 251/258
2007
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CHEMICAL EQUILIBRIUM CONSTRAINTS ON HYDROTHERMAL FLUID COMPOSITION: REACTION OF SEAWATER AND METEORIC WATER WITH BASALT AND PERIDOTITE
T226 Diversity in Crustal Fluid Compositions: Geological Origins and ConsequencesWednesday, 31 October 20071:30 PM - 5:30 PM
2005
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THE BUTTE HYDROTHERMAL SYSTEM: ONE MAGMATIC FLUID YIELDED ALL VEIN TYPES
T138 Sources of Porphyry Copper Deposits: Magmas, Metals, and Fluids IITuesday, 18 October 20058:00 AM - 12:00 PM