Petrologic Constraints on Mantle Temperature and Water Content

Slides:



Advertisements
Similar presentations
Radiogenic isotopic evolution of the mantle and crust Matt Jackson and Bill McDonot.
Advertisements

Subduction Factory: Its Role in the Evolution of the Solid Earth Y
Slab-mantle decoupling and its implications for subduction zone thermal structure, fluid supply, and geophysical processes Ikuko Wada1,2 and Kelin Wang1,2.
Determining the nature of the LLSVP CIDER Workshop 2012 Maxim Ballmer, Jamie Barron, Rohan Kundargi, Curtis Williams, Rick Carlson, Jasper Konter, Jackie.
Conclusions… Challenge: 1)Seismic waves are affected by variations in temperature, pressure, composition, mineralogy, structure (layering, scales and distribution.
1; movies Topography of a fast spreading ridge (EPR)
Lecture 4: MORB petrogenesis
Silicate Earth Primitive mantle Present-day mantle Crust Oceanic crust Continental crust Reservoir Volume Mass Mass % (10 27 cm 3 )(10 27 g) Earth
WHAT IS MAGMA MADE UP OF?. At divergent boundaries and hot spots, magma forms by PARTIAL MELTING (not complete melting) of the mantle Minerals with higher.
08/09/2007VLab-workshop1 Geophysical Anomalies in the Central Pacific Upper Mantle Implications for Water Transport by a Plume Shun-ichiro Karato Yale.
1 SUMMARY OF MANTLE TEMPERATURES DON L. ANDERSON 2006.
Compositional Model for the Mantle beneath the Pacific Plate Rhea Workman Outline: 1. Concepts of trace element and isotope geochemistry for the Earth’s.
Lecture-10 1 Lecture #10- Subduction Zones. Lecture-10 2 Subduction Zones F When two tectonic plates converge often one will get buried or subducted beneath.
Melts+Fluids in the Mantle *Silicate Melts *Hydrous Fluids *CO2 vapor (also CH4-rich vapor?) *Carbonatites *Halide Melts (brines) *Sulfide/oxysulfide melts.
Hydrous partial melting of the upper mantle as judged from mineral/melt partition coefficients Marc M. Hirschmann Cyril Aubaud Tony Withers University.
The Transition Zone and Uppermost Lower Mantle in Subduction Zones Justin Revenaugh Anna Courtier Geology and Geophysics University of Minnesota.
Outline 1.Properties of silicate liquids 2.Adiabatic decompression melting Melting temperature(s) of lherzolite Model for mid-ocean ridges 3.Melting in.
What is the role of Subduction in Deep Earth Volatile Cycles? Marc Hirschmann University of Minnesota.
Volatile Recycling at Subduction Zones Terry Plank, Lamont Doherty Earth Observatory The Subduction Factory.
Origin of Basaltic Magma
Dept. Earth SciencesJ. Huw Davies, Hydrofrac Model Davies, Nature, 1999.
L=A  -r Dynamic recrystallization. Some Applications Dewatering due to partial melting and the lithosphere-asthenosphere structure (Karato.
A low velocity layer (LVZ) at the top of the subducting plate has been detected in a majority of subduction zones. LVZ may be a hydrated layer of oceanic.
Composition of the Earth: a more volatile elements perspective Cider 2010 Bill McDonough Geology, University of Maryland Support from:
Are the predictions of the plume hypothesis borne out by observation? 1.Temperature Natalie Starkey.
Are ‘hotspots’ ‘wetspots’? By Clare de Villanueva, 4 th yr F601.
Past, Present and Future What have we learned? -Mantle and Plates are an intimately coupled system -Deep mantle structure is important for the surface.
On the Role of Water in Diverging Planetary Geodynamics some preliminary results Peter van Thienen and Philippe Lognonn é Département de Géophysique Spatiale.
Kimberlites, Carbonatites and diamonds
Structural Transitions in Amorphous Mantle Phases Dan Shim Massachusetts Institute of Technology Thanks to: K. Catalli, T. Grove, NSF CIDER 2004.
The Influence of Magma Ocean Processes on the Present-day Inventory of Deep Earth Carbon Rajdeep Dasgupta CIDER post-AGU workshop December 10, 2011.
Melting Regions of the Mantle Terry Plank: LDEO with C-T. Lee (Rice) D. Forsyth (Brown) E. Hauri (Carnegie ) K.Fischer (Brown) G. Abers (LDEO) D.Wiens.
Experimental constraints on subduction-related magmatism : Hydrous Melting of upper mantle perdotites Modified after a ppt by Peter Ulmer (Blumone, Adamello,
Initiation and preservation of localized deformation in the mantle
Seismological observations Earth’s deep interior, and their geodynamical and mineral physical interpretation Arwen Deuss, Jennifer Andrews University of.
Water in the Mantle ? Can be stored: 1)Hydrous minerals - only stable shallow 2) Dissolved in normally anhydrous minerals 3)A hydrous silica-rich fluid.
The Ongoing and the Early Differentiation of the Earth: the Role of Volatiles Rajdeep Dasgupta June 26, 2008COMPRES.
Dynamics of Planetary Interiors
Seismological studies on mantle upwelling in NE Japan: Implications for the genesis of arc magmas Junichi Nakajima & Akira Hasegawa Research Center for.
Melting processes and volatile fluxes at the Gakkel Ridge – do ultra-slow spreading systems reveal insights to Rift evolution? Alison Shaw, Mark Behn,
Oceanic Spreading Centers. Structure of a fast spreading center (East Pacific Rise ~ 10 cm/yr)
What is the origin of OIB? John Caulfield Identification and explanation of similarities and differences in isotopic ratios (Sr, Nd, Os, O and Pb) between.
Structure of the Earth and Mineralogy Environmental Science Earth Science Unit Environmental Science Earth Science Unit.
Magmas Best, Ch. 8. Constitution of Magmas Hot molten rock T = degrees C Composed of ions or complexes Phase –Homogeneous – Separable part.
Links between melting, rheology and the composition and structure of the upper mantle Greg Hirth, Brown Univeristy Marc Parmentier & Alberto Saal Mark.
MAGE postdoc presentation - MAGE midterm meeting Peter van Thienen D épartement de Géophysique Spatiale et Planétaire, Institut de Physique du Globe de.
Carbon Cycling in Subduction Zones implications for mantle-exosphere exchange Rajdeep Dasgupta.
Mantle Melting Some slides from Mary Leech. Table A Classification of Granitoid Rocks Based on Tectonic Setting. After Pitcher (1983) in K. J. Hsü.
 FMQ Arc lavas Arc-related xenoliths Cascades central Mexico Hornblende-rich xenoliths Ichinomegata, Japan Izu-Bonin, Japan Lihir, Papua.
What is the thermal structure of a subduction zone?
C OUPLING THE D EEP C ARBON AND S ULFUR C YCLES – I MPLICATIONS FOR THE O RIGIN AND S TORAGE OF D EEP E ARTH V OLATILES Rajdeep Dasgupta CIDER Community.
Pop Quiz! 1.__ 2.__ 3.__ 4.__ 5.__ 6.__ 7.__ 8.__ Inner Core Mantle Mesosphere Outer Core Asthenosphere Ocean Crust Lithosphere Continental Crust.
217/15-1 (Lagavulin) 2.6 km section of basalts Lower depleted picrites (low TiO2 MORB) Upper “FIBG” enriched basalts (high TiO2) Major unconformity.
Non-Traditional Isotope Laboratory
Island Arc Magmatism Eruption of Anatahan Volcano,
Geol 2312 Igneous and Metamorphic Petrology
Geol 2312 Igneous and Metamorphic Petrology
Squeezing the Slab: future directions for metamorphic petrology in the SZO Andrew Smye Sentence about metamorphic petrology and need to link observations.
Original artwork by Gary Hincks
Rajdeep Dasgupta Department of Earth Science, Rice University
Ocean-Ocean Subduction Zones System
Carbonates in mantle xenoliths from the French Massif Central:
Length scale of heterogeneity
Mantle wedge processes
Mantle wedge processes
Estimating mantle temperature and composition
Plate Tectonics.
Eclogites, metamorphism and plate tectonics
Igneous Rock Notes.
Shun-ichiro Karato Partial melting, water, rheological properties
Presentation transcript:

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

Stixrude&Lithgow-Bertelloni, 2005

Stixrude&Lithgow-Bertelloni, 2005

Oceanic Crust Production Langmuir et al., 1992; Asimow et al., 2001

Trace amounts of H2O enhance melting…. Hirth & Kohlstedt, 1996; Asimow & Langmuir, 2003

Saal et al., 2002 MORB and seamount glasses Easter Microplate CO2 (wt.%) Kingley et al. 2002 H2O (wt.%)

H2O Storage Capacity

Hirth & Kohlstedt, 1996

Aubaud et al., GRL, 2004

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

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

Dasgupta & Hirschmann (2006) - Nature

Carbonated Melt Catalyzes Grain Growth Subsolidus Supersolidus Dasgupta et al., 2004 Dasgupta et al. (2004) - EPSL

Dasgupta & Hirschmann (2006) - Nature

Origin of Chemical Lithosphere and Volatile induced Melting of Peridotite Hirth & Kohlstedt (1996) Aubaud et al., 2004 Peridotite Dehydration is aided by Partial Melting

Dasgupta & Hirschmann (2006) - Nature

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)

Deep Carbonated Silicate Melting & H2O Extraction Beneath Ridges

Schmidt+Poli, 1998

Honshu - Van Keken, 2003

(from Gaetani+Grove, 2003)

Tim Grove - unpublished results (thanks, Tim!)

High Temperature Melt or Fluid Transfer from the Slab Elliott, 2003

Kelemen et al. 2003

Davies&Stevenson, 1992 Mibe et al., 2001

Temperatures at the base of the crust based on metamorphic thermobarometry Kelemen et al., 2003

Mt. Shasta-Medicine Lake (Elkins Tanton et al., 2001)

Thanks for listening…..