Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of...

40
Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota

Transcript of Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of...

Page 1: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.

Petrologic Constraints on Mantle Temperature and

Water ContentMarc Hirschmann

University of Minnesota

Page 2: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.

Stixrude&Lithgow-Bertelloni, 2005

Page 3: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.

Stixrude&Lithgow-Bertelloni, 2005

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Oceanic Crust Production

Langmuir et al., 1992; Asimow et al., 2001

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Trace amounts of H2O enhance melting….

Hirth & Kohlstedt, 1996; Asimow & Langmuir, 2003

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Saal et al., 2002

H2O (wt.%)

CO

2 (w

t.%

)

MORB and seamount glassesEaster Microplate

Kingley et al. 2002

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H2O Storage Capacity

Page 8: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.
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Hirth & Kohlstedt, 1996

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Aubaud et al., GRL, 2004

Page 15: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.

Hirth & Kohlstedt, 1996 Aubaud et al., GRL, 2004

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0

50

100

150

200

250

0 200 400 600 800 1000 1200

H2O (ppm wt.)

Initial depth of melting (km)

1550 °C

1450 °C

1350 °C

RIDGE

PLUME

Tp

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MELT Experiment beneath EPR

The MELT Seismic Team (1998)Gu et al. (2005)

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Dasgupta & Hirschmann (2006) - Nature

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Carbonated Melt Catalyzes Grain Growth

Subsolidus Supersolidus

Dasgupta et al. (2004) - EPSLDasgupta et al., 2004

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Dasgupta & Hirschmann (2006) - Nature

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Origin of Chemical Lithosphere and Volatile induced Melting of PeridotiteHirth & Kohlstedt (1996)

Aubaud et al., 2004

Peridotite Dehydration is aided by Partial Melting

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Dasgupta & Hirschmann (2006) - Nature

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Deep Carbonated Silicate Melting Beneath Ridges

Transition from

carbonatite to carbonated

silicate melts at 3 GPa

Silicate Melting is

enhanced in presence of

carbonate

Dasgupta & Hirschmann (submitted)

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Page 26: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.

Deep Carbonated Silicate Melting & H2O Extraction Beneath Ridges

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Schmidt+Poli, 1998

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Honshu - Van Keken, 2003

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(from Gaetani+Grove, 2003)

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QuickTime™ and aTIFF (Uncompressed) decompressor

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Tim Grove - unpublished results(thanks, Tim!)

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Elliott, 2003

High Temperature Melt or FluidTransfer from the Slab

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Kelemen et al. 2003

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QuickTime™ and aTIFF (Uncompressed) decompressor

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QuickTime™ and aTIFF (Uncompressed) decompressor

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Davies&Stevenson, 1992 Mibe et al., 2001

QuickTime™ and aTIFF (Uncompressed) decompressor

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Kelemen et al., 2003

Temperatures at the baseof the crust based onmetamorphic thermobarometry

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(Elkins Tanton et al., 2001)

Mt. Shasta-Medicine Lake

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High Temperatures in Arcs- Petrologic Evidence Location Max T

(°C) P

(GPa) Method So urce

Banda 1320 1.2 Melt Inclus ions

Sisson&Bronto, 1998

Cascades 1450 2.2 Inverse Exper iments

Elkins Tanton e t a l., 2001

Japan 1320 -1360

1.7 -2.3 Inverse Exper iments

Tatsu mi et a l. 1983

Japan 1325 1.2 Inverse Exper iments

Kush iro, 1987

N. Tonga 1480 1.5 Inverse Exper iments

Fa lloon&Danyus hevsky,200 0

Aleut ians 1300 1.2 Inverse Exper iments

Draper & Jo hnston, 1991

Page 40: Petrologic Constraints on Mantle Temperature and Water Content Marc Hirschmann University of Minnesota.

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