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in the genesis of andesite
The role of H2O in the genesis of andesite Kayla Iacovino NASA Space Grant Symposium April 19th, 2008 Picture: Mt. Yasur Thanks to: Dr. Gordon Moore, Dr. Kurt Roggensack Dr. John Holloway, and Depths of the Earth Lab
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Outline What is andesite, and why is it important?
Can andesite originate in the mantle? Is H2O important? Experimental methods Results and implications
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Defining andesite Andesite Type locality: Andes of S. America
Intermediate volcanic rock (58-62 wt% SiO2) Associated with continental subduction zones
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Subduction Zones and Andesites
Water brought by subduction into the mantle.
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Andesites from the mantle?
Typically, mantle magmas are basaltic (<52 wt% SiO2) Silica-rich magmas not typically in chemical equilibrium with mantle minerals (olivine, orthopyroxene) Evidence for mantle andesite Andesite composition lava found with mantle xenoliths (Blatter & Carmichael, 1998) Si rich = andesite. This observation is inconsistent with what we know about the chemistry. How can we explain this observation if we know that andesites are not in chemical equilibrium with mantle minerals?
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Hypothesis Water effects the andesite magma chemistry such that it can be in equilibrium with mantle minerals Mg2SiO4 + SiO2 = Mg2Si2O6 Evidence Hydrous minerals (hornblende) in xenoliths Water brought by slab during subduction Test hypothesis with high-pressure and temperature experiments (500MPa, 1190°C) Olivine melt Pyroxene
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Methods The Piston Cylinder Non-End Loaded “Sandwich” The Assembly
The Capsule AuPd ~ 0.25’’ The Piston Cylinder
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Results Several experiments with varying water contents
H2O contents estimated from probe totals melt opx bread xtallizing opx opx xtallizing ol melt 950x 350x Low H2O ~1 wt% High H2O ~3 wt%
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Implications Water does affect mineral-melt equilibrium
Crystallizing phases change with varying water content Low water content experiments show no signs of crystallizing olivine Presence of H2O (≥~3 wt%) can explain equilibrium between an andesitic melt and mantle minerals
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Thank you
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