Constraints on Mantle Composition from 1D Earth Models 2007 Vlab/EGC Workshop ESS Building SUNY Stony Brook Stony Brook, NY 11794 Baosheng Li Supported.

Slides:



Advertisements
Similar presentations
SPP 1257 Modelling of the Dynamic Earth from an Integrative Analysis of Potential Fields, Seismic Tomography and other Geophysical Data M. Kaban, A. Baranov.
Advertisements

7/12/04CIDER/ITP Short Course Composition and Structure of Earth’s Interior A Perspective from Mineral Physics.
Folie 1 Physical State of the Deep Interior of CoRoT-7b F. W. Wagner T. Rückriemen F. Sohl German Aerospace Center (DLR) IAU Symposium October.
The Transition Zone: Slabs ’ Purgatory CIDER, Group A Garrett Leahy, Ved Lekic, Urska Manners, Christine Reif, Joost van Summeren, Tai-Lin Tseng,
Conclusions… Challenge: 1)Seismic waves are affected by variations in temperature, pressure, composition, mineralogy, structure (layering, scales and distribution.
Constraints on the LAB from Seismology, Petrology and Geodynamics/Mineral Physics fundamentals/10h.html A. Bengston, M. Blondes,
Single-crystal elasticity of hydrous wadsleyite and implication for the Earth’s transition zone Zhu Mao 1, Steven D. Jacobsen 1, Fuming Jiang 1, Joseph.
The Earth’s Structure Seismology and the Earth’s Deep Interior The Earth’s Structure from Travel Times Spherically symmetric structure: PREM - Crustal.
High Pressure Mineralogy Minerals Methods & Meaning High Pressure Mineralogy.
Thermoelastic properties of ferropericlase R. Wentzcovitch Dept. of Chemical Engineering and Materials Science, Minnesota Supercomputing Institute J. F.
Europa Scenarios: Physical Models Ice-cracks on surface consistent with either “warm-ice” or water beneath the surface Near infrared mapping consistent.
Inner Core Outer Core Lower Mantle Upper Mantle Crust Moho 6371Km 5000Km 2900 Km 0 Km 1050 Km asthenosphere Gutenburg Moho boundary is between 25 and.
Global Distribution of Crustal Material Inferred by Seismology Nozomu Takeuchi (ERI, Univ of Tokyo) (1)Importance of Directional Measurements from geophysicists’
2:57 PM, Dec. 8, 2012 CIDER Post-AGU 2012 “Snowfall” in F Layer Jie (Jackie) Li University of Michigan Advanced Photon Source.
1 Composition of the Earth GLY 4200 Fall, Interior of the Earth Earth’s interior is divided into zones, with differing properties and compositions.
Lowermost Outer Core and the ICB Bin Chen, Vernon Cormier, Shan Dou, Garrett Euler, Lili Gao, David Gubbins, Kuang He, Svetlana Kharlamova, Jie Li, Hongfeng.
Constraining the composition and thermal state of the Moon from inversion of seismic velocities Oleg Kuskov, Victor Kronrod, Ecaterina Kronrod Vernadsky.
Seismic tomography Tomography attempts to determine anomalous structures within the Earth as revealed by deviations from “average” seismic properties at.
Igneous Petrology John Winter.
3D seismic imaging of the earth’s mantle Barbara Romanowicz Department of Earth and Planetary Science U.C. Berkeley.
How well do we know density in the Earth?. Velocity in the Earth is well known.
Computer Aided Tomography Tomos: cut (Gr.) Extensively used to find 3D structure from surface measurements (X-ray, sound, seismic waves)
LAYERS OF THE EARTH HOW WE KNOW ABOUT THE DEEP INTERIOR: Meteorites Seismic Waves Magnetic Field Gravity.
Earth’s internal structure: a seismologist’s view.
Igneous Petrology John Winter. The Earth’s Interior Crust: Oceanic crust Thin: 10 km Relatively uniform stratigraphy = ophiolite suite: = ophiolite suite:
Mineral physics and seismic constraints on Earth’s structure and dynamics Earth stucture, mineralogy, elasticity.
First Principles Thermoelasticity of Minerals: Insights into the Earth’s LM Problems related with seismic observations T and composition in the lower mantle.
1 Rocks and the Earth’s Interior GLY Summer 2015 Lecture 6.
Department of Geology & Geophysics
Renata M. Wentzcovitch Dept. of Chemical Engineering and Materials Science, Minnesota Supercomputing Institute UNIVERSITY OF MINNESOTA Phase transitions.
Chemical and Clapeyron- induced buoyancy at the 660 km discontinuity D.J. Weidner & Y. Wang 1998.
Phase Transitions in the Earth’s Mantle
Probing Earth’s deep interior using mantle discontinuities Arwen Deuss University of Cambridge, UK also: Jennifer Andrews, Kit Chambers, Simon Redfern,
Seismological observations Earth’s deep interior, and their geodynamical and mineral physical interpretation Arwen Deuss, Jennifer Andrews University of.
Fluid, 90% iron solidified iron km ,00012,000 Mg(Fe) silicates phase changes basaltic-granitic crust chemical stratification and differentiation.
Direct Pressure Measurements and Insights on Current Pressure Scales Baosheng Li ESS Building SUNY Stony Brook Stony Brook, NY This research is supported.
Global seismic tomography and its CIDER applications Adam M. Dziewonski KITP, July 14, 2008.
1 Petrology Lecture 6 Generation of Basaltic Magma GLY Spring, 2012.
Beyond Elasticity stress, strain, time Don Weidner Stony Brook.
Plate Tectonics.
Seismological studies on mantle upwelling in NE Japan: Implications for the genesis of arc magmas Junichi Nakajima & Akira Hasegawa Research Center for.
Adam M. Dziewonski in cooperation with Ved Lekic and Barbara Romanowicz Terra Incognita Again ; Five zones in the mantle KITP July 19, 2012.
BurnMan: A Lower Mantle Toolbox Valentina Magni (Durham) Timo Heister (Texas A&M) Sanne Cottar (Berkeley) Marc Hirschmann (Minnesota) Ian Rose(Berkeley)
1 Composition of the Earth GLY 4200 Fall, Interior of the Earth Earth’s interior is divided into zones, with differing properties and compositions.
Structure and chemistry of the Earth Today’s topic: The chemistry of Earth’s mantle and crust.
The Core and Mantle: future prospects for understanding the Deep Earth
Constraints on the observation of mantle plumes using global seismology Arwen Deuss University of Cambridge, UK.
First Principles Thermoelasticity of Mantle Minerals Renata M. M. Wentzcovitch Department of Chemical Engineering and Materials Science U. of Minnesota,
First Principles Thermoelasticity of Minerals: Insights into the Earth’s LM Seismic observations and the nature of the LM T and composition in the lower.
Constraints on transition zone discontinuities from surface wave overtone measurements Ueli Meier Jeannot Trampert Andrew Curtis.
Geology 5640/6640 Introduction to Seismology 13 Apr 2015 © A.R. Lowry 2015 Read for Wed 15 Apr: S&W (§3.6) Last time: Ray-Tracing in a Spherical.
Structure of Earth as imaged by seismic waves
Spin Transitions in Lower Mantle Minerals? Concentrate on ferropericlase as more likely to have a big effect.
The Core-Mantle Boundary Region Jeanloz & Williams, 1998 Lower mantle Outer core CMB Heat flow.
Structure of the Earth.
The formation of MORB vs Ophiolites Anneen Burger Anhydrous Melting of Peridotite at 0-15 Kb Pressure and the Genesis of Tholeiitic Basalts A.L. Jaques.
Geology 5640/6640 Introduction to Seismology 11 Feb 2015 © A.R. Lowry 2015 Last time: Seismology as Investigative Tool Deep-Earth investigations use earthquakes.
How has seismic study given us a model of earth’s crust and interior?
Rocks and the Earth’s Interior
The Rock Cycle.
Fundamental Concepts GLY 4310 Spring, 2013
Transition Zone Discontinuities
Seismic velocity gradients across the transition zone
CIDER/ITP Short Course
We have been talking about minerals primarily in the earth’s crust
Seismic tomography Tomography attempts to determine anomalous structures within the Earth as revealed by deviations from “average” seismic properties at.
Eh Tan CIG at CIDER Workshop 2009
Asthenosphere flow and mantle lithosphere instabilities below continental rifts and rifted margins Jolante van Wijk (University of Houston) Jeroen van.
We have been talking about minerals primarily in the earth’s crust
Earth’s Interior.
Presentation transcript:

Constraints on Mantle Composition from 1D Earth Models 2007 Vlab/EGC Workshop ESS Building SUNY Stony Brook Stony Brook, NY Baosheng Li Supported by National Science Foundation

Structure of the Earth Upper mantle and Transition Zone: Low velocity zone, discontinuities; Lower Mantle: Phase transition at D” PREM Dziewonski and Anderson (1981) MantleOCIC

(Ringwood, 1975) Mineralogy and Chemical Composition Models of the Mantle

Thermoelasticity for mantle minerals/phases Mineral Assemblage in the mantle Adiabatically or isothermally raise pressure to deeper depths Mixing of all phases (VRH, HS, etc) Constraints on the Earth’s Interior: Forward Modelling

Bass and Anderson (1984) Composition: Pyrolite and Piclogite

Bass and Anderson (1984) Blue: Piclogite ; Red: Pyrolite

Comparison of the P and S wave velocities for olivine and wadsleyite at 410 km depth W. Liu, J. Kung and B. Li (GRL,2005) Duffy and Anderson (JGR, 1989)

Thermoelasticity of Mantle Minerals Stixrude and Lithgow-Bertelloni (2005)

Velocity of Mantle Minerals at Mantle Depths B. Li and R. C. Liebermann (PNAS, 2007)

Phase Fraction of Pyrolite in the Mantle Stixrude and Lithgow-Bertelloni (2005)

Phase Assemblage of Piclogite in the Mantle Stixrude and Lithgow-Bertelloni (G J I, 2005)

B. Li and R. C. Liebermann (PNAS, 2007)

Ita and Stixrude (1992) PREM Pyrolite Piclogite Blue: 1500K Red: 1600K Stixrude and Lithgow-Bertelloni (2005)

Comparison of Pyrolite with 1-D PREM/AK135 Simultaneous Vp, Vs,  comparison for tight constraints B. Li and J. Zhang (PEPI, 2005) See also Zhao&Anderson (1994), Jackson (1998) Hamma and Anderson (2002); Stacey(1996); Murakami et al(2007)