Mantle Convection and Surface Expressions

Mantle Convection and Surface Expressions
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A multidisciplinary perspective on the dynamic processes occurring in Earth's mantle The convective motion of material in Earth's mantle, powered by heat from the deep interior of our planet, drives plate tectonics at the surface, generating earthquakes and volcanic activity. It shapes our familiar surface landscapes, and also stabilizes the oceans and atmosphere on geologic timescales. Mantle Convection and Surface Expressions brings together perspectives from observational geophysics, numerical modelling, geochemistry, and mineral physics to build a holistic picture of the deep Earth. It explores the dynamic processes occurring in the mantle as well as the associated heat and material cycles. Volume highlights include: Perspectives from different scientific disciplines with an emphasis on exploring synergies Current state of the mantle, its physical properties, compositional structure, and dynamic evolution Transport of heat and material through the mantle as constrained by geophysical observations, geochemical data and geodynamic model predictions Surface expressions of mantle dynamics and its control on planetary evolution and habitability The American Geophysical Union promotes discovery in Earth and space science for the benefit of humanity. Its publications disseminate scientific knowledge and provide resources for researchers, students, and professionals.

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Table of Contents

List of Tables

List of Illustrations

Guide

Pages

Geophysical Monograph Series

Geophysical Monograph 263. Mantle Convection and Surface Expressions

Dedication

LIST OF CONTRIBUTORS

PREFACE

Part I: State of the Mantle: Properties and Dynamic Evolution

Part II: Material Transport Across the Mantle: Geophysical Observations and Geodynamic Predictions

Part III: Surface Expressions: Mantle Controls on Planetary Evolution and Habitability

1 Long‐Wavelength Mantle Structure: Geophysical Constraints and Dynamical Models

ABSTRACT

1.1 INTRODUCTION

1.2 METHODS. 1.2.1 Mantle Tomography

1.2.2 Mantle Circulation Models

1.2.3 Inversions for Viscosity

1.3 RESULTS

1.4 DISCUSSION

1.5 CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

2 Experimental Deformation of Lower Mantle Rocks and Minerals

ABSTRACT

2.1 INTRODUCTION

2.2 BACKGROUND

2.3 METHODS: EXPERIMENTAL DEFORMATION OF LOWER MANTLE MINERALS

2.3.1 The Diamond Anvil Cell as a Deformation Device

2.3.2 Large‐Volume Deformation Devices

2.3.3 Texture and Strength Measurements in High‐Pressure Experiments

2.3.4 A Note on Scaling Experiments to the Lower Mantle

2.4 DEFORMATION STUDIES OF LOWER MANTLE PHASES

2.4.1 Differential Stress Measurements in Lower Mantle Phases

Ferropericlase

CaSiO3 Perovskite

Bridgmanite

Post‐Perovskite

2.4.2 Textures and Slip Systems in Lower Mantle Phases

Ferropericlase

CaSiO3 Perovskite

Deformation of Bridgmanite

2.4.3 Post‐Perovskite

2.5 POLYPHASE DEFORMATION

2.5.1 Stress and Strain Partitioning in Polyphase Aggregates

2.5.2 Differential Stresses in High Pressure Studies of Polyphase Aggregates

2.5.3 Texture Development in Polyphase Materials

2.5.4 Texture Development in High Pressure Studies of Polyphase Aggregates

2.6 IMPLICATIONS

2.7 CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

3 Seismic Wave Velocities in Earth’s Mantle from Mineral Elasticity

ABSTRACT

3.1 INTRODUCTION

3.2 ELASTIC PROPERTIES

3.3 EXPERIMENTS

3.4 COMPUTATIONS

3.5 PARAMETER UNCERTAINTIES

3.6 ELASTIC PROPERTIES OF SOLID SOLUTIONS

3.7 ELASTIC ANOMALIES FROM CONTINUOUS PHASE TRANSITIONS

3.8 EARTH’S LOWER MANTLE

3.9 CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

4 From Mantle Convection to Seismic Observations: Quantifying the Uncertainties Related to Anelasticity

ABSTRACT

4.1 INTRODUCTION

4.2 FROM GEODYNAMIC HYPOTHESIS TO SEISMIC OBSERVATIONS

4.2.1 Predicting Seismic Mantle Structure

Mantle Evolution and the Present‐Day Temperature Field

Relating Temperatures to Seismic Velocities

4.2.2 Predicting Seismic Observables – Truly “Synthetic” Data

4.2.3 Linking to Earth Observations – The Importance of Uncertainties

4.3 CONSIDERING MINERALOGICAL UNCERTAINTIES

4.3.1 Anelasticity – A Crucial Factor for Traveltime Uncertainty

Frequency and Temperature Dependence of Q

Anelasticity Correction of Seismic Velocities

4.4 QUANTIFYING THE EFFECTS OF UNCERTAINTIES RELATED TO ANELASTICITY

4.5 SUMMARY AND CONCLUDING REMARKS

ACKNOWLEDGMENTS

REFERENCES

5 Geochemical Diversity in the Mantle

ABSTRACT

5.1 INTRODUCTION

5.2 DEFINITIONS AND INTERPRETATIONS OF DISTINCT MANTLE COMPONENTS

5.2.1 Depleted Mantle Component

5.2.2 Enriched Mantle Component

5.2.3 HIMU Mantle Component

5.2.4 FOZO and Primordial Mantle Components

5.3 LITHOLOGICAL ASPECTS OF THE MANTLE COMPONENTS

5.4 THE ROLE OF CARBONATE IN MANTLE GEOCHEMICAL HETEROGENEITY

5.5 RECENT PROGRESS AND OUTLOOK FOR THE MANTLE EVOLUTION

5.5.1 Nontraditional Stable Isotopes as New Proxies to Trace Recycling

5.5.2 Volatile Recycling

5.5.3 Ancient Surface Environments and Mantle Evolution

ACKNOWLEDGMENTS

REFERENCES

6 Tracking the Evolution of Magmas from Heterogeneous Mantle Sources to Eruption

ABSTRACT

6.1 INTRODUCTION

6.2 PARTIAL MELTING OF A HETEROGENEOUS MANTLE. 6.2.1 Contribution of Mantle Lithologies to Magma Genesis

6.3 PERIDOTITE VS. PYROXENITE: EXPERIMENTAL MELT COMPOSITIONS. 6.3.1 Major Elements

6.3.2 First Row Transition Elements

6.4 INTERACTIONS BETWEEN CHEMICAL HETEROGENEITIES AND PERIDOTITE

6.5 SAMPLING MELTS OF THE MANTLE: APPROACH AND OVERVIEW

6.5.1 MORBs. Intracrustal Processing

Natural MORBs and Their Cumulates

Primary MORBs

6.5.2 Ocean Island Basalts

Source Lithologies of Primitive OIBs

Natural OIB and Their Cumulates

6.5.3 Arc Magmas. Arc Magma Genesis – A Complexity of Factors

Experimental Perspectives on Primary Arc Magma Generation: Melting of the Peridotitic Mantle Wedge

Melting of Nonperidotitic Sources in Arc Magma Generation. Downgoing plate contributions to fluid flux and sediment melt diapirs

Upper plate processes

Natural Arc Magmas and Their Cumulates

6.6 FUTURE DIRECTIONS

ACKNOWLEDGMENTS

REFERENCES

7 Super‐Deep Diamonds: Emerging Deep Mantle Insights from the Past Decade

ABSTRACT

7.1 INTRODUCTION

7.2 OCEAN CRUST AND CARBON RECYCLED TO THE LOWER MANTLE

7.3 RECOGNIZING CARBONATITIC MELT SIGNATURES IN THE DEEP MANTLE

7.4 SIGNS OF DEEP WATER

7.5 PRESERVED DEEP MANTLE MINERALS WITH ORIGINAL CRYSTAL STRUCTURE

7.6 NEW KINDS OF SUPER‐DEEP DIAMONDS: CLIPPIR AND TYPE IIB DIAMONDS

7.7 A REDUCED IRON‐SATURATED SUBLITHOSPHERIC MANTLE

7.8 DISCUSSION

ACKNOWLEDGMENTS

REFERENCES

8 Seismic and Mineral Physics Constraints on the D" Layer

ABSTRACT

8.1 INTRODUCTION

8.2 THE D" REFLECTOR(S) 8.2.1 Visibility of the Reflection

8.2.2 Travel Times of the Reflection(s)

8.2.3 Amplitude and Polarity of the Reflection(s)

8.2.4 Plausible Explanations

8.2.5 Case Study: Observations and Interpretations of D" Underneath the Northern Pacific Region

8.3 ULTRALOW VELOCITY ZONES. 8.3.1 Seismic Observations

8.3.2 Plausible Explanations

Partial Melt

Extreme Chemical or Phase Heterogeneity

Anisotropy

8.3.3 Inversion of Iron‐Rich Phase Assemblages with Seismic Observations

ULVZ Case 1: Europe and Western Asia

ULVZ Case 2: NW America

ULVZ Case 3: Central America

ULVZ Case 4: Coral Sea

ULVZ Case 5: Anisotropy

8.3.4 ULVZ Topography

8.3.5 Summary of ULVZ Case Studies

8.4 SUMMARY AND CONCLUSIONS

ACKNOWLEDGMENTS

APPENDIX

REFERENCES

9 Toward Consistent Seismological Models of the Core–Mantle Boundary Landscape

ABSTRACT

9.1 INTRODUCTION

9.2 EXISTING MODELS OF CMB TOPOGRAPHY

9.2.1 Regional CMB Topography Studies

9.2.2 Global Body‐Wave Models of CMB Topography

9.2.3 CMB Topography Constrained by Normal Modes

9.2.4 Other Constraints on CMB Topography

9.2.5 Dynamic Predictions of CMB Topography

9.3 TWENTY YEARS OF DENSITY MODELS

9.3.1 Early Normal‐Mode Studies

9.3.2 Recent Studies Utilizing Improved Data Sets

9.3.3 New Developments in Density Studies

9.4 QUANTITATIVE ASSESSMENT OF EXISTING SEISMOLOGICAL MODELS

9.4.1 Cross‐Model Correlation

9.4.2 Average Models

9.4.3 Vote Maps of Density and CMB Topography

9.4.4 Comparison to Geodynamic Predictions

9.4.5 Summary of Current Model Features

9.5 EFFORTS TOWARD MORE CONSISTENT MODELS

9.5.1 Factors Influencing the Interpretation of Density Models

9.5.2 Future Development of Density Models

9.5.3 Developing Consistent CMB Topography Models

9.5.4 Integrating Seismology With Other Constraints

9.6 CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

10 Dynamics of the Upper Mantle in Light of Seismic Anisotropy

ABSTRACT

10.1 INTRODUCTION

10.2 OBSERVATIONS OF SEISMIC ANISOTROPY

10.2.1 Pn Anisotropy

10.2.2 Shear Wave Splitting

10.2.3 Surface Waves

10.3 INTERPRETATION OF SEISMIC ANISOTROPY. 10.3.1 Origin of Upper Mantle Anisotropy

10.3.2 Anisotropy and Plate Motions

10.3.3 Mantle Circulation Modeling

Boundary Layer Anisotropy

10.3.4 Examples of Inferences That Extend Beyond the Reference Model

10.4 OPEN QUESTIONS. 10.4.1 Regional Complexities and Scale‐Dependent Resolution

Oceanic Plates Revisited

Anisotropy in Continents

10.4.2 Uncertainties About Microphysics. Formation of Olivine LPO

Mechanical Anisotropy

10.5 WAYS FORWARD

10.6 CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

11 Mantle Convection in Subduction Zones: Insights from Seismic Anisotropy Tomography

ABSTRACT

11.1 INTRODUCTION

11.2 METHOD

11.2.1 Azimuthal Anisotropy Tomography

11.2.2 Radial Anisotropy Tomography

11.3 APPLICATIONS

11.3.1 Northwest Pacific

11.3.2 Southeast Asia

11.3.3 New Zealand

11.3.4 Alaska

11.3.5 North America

11.3.6 Europe

11.4 DISCUSSION. 11.4.1 Surface‐Wave Anisotropic Tomography

11.4.2 Shear‐Wave Splitting Tomography

11.4.3 Anisotropic Tomography: What Can We Learn and Expect?

11.5 CONCLUSIONS

ACKNOWLEDGMENTS

REFERENCES

12 The Cycling of Subducted Oceanic Crust in the Earth’s Deep Mantle

ABSTRACT

12.1 INTRODUCTION

12.2 OBSERVATIONAL CONSTRAINTS ON THE DISTRIBUTION OF OCEANIC CRUST IN THE DEEP MANTLE. 12.2.1 Geochemical Observations

12.2.2 Seismic Observations

12.3 THE CYCLING OF SUBDUCTED OCEANIC CRUST IN THE DEEP MANTLE

12.3.1 The Separation of Slab Components at the Base of Transition Zone

12.3.2 The Accumulation of Subducted Oceanic Crust on the CMB

12.3.3 Stability and Entrainment of the Crustal Accumulations on the CMB

12.3.4 The Fate of the Entrained Oceanic Crust

12.4 SUMMARY AND FUTURE WORK

12.5 ACKNOWLEDGMENTS

REFERENCES

13 Toward Imaging Flow at the Base of the Mantle with Seismic, Mineral Physics, and Geodynamic Constraints

ABSTRACT

13.1 INTRODUCTION

13.2 OBSERVATIONAL CONSTRAINTS ON LOWERMOST MANTLE FLOW. 13.2.1 Global Tomographic Models

13.2.2 Regional Body‐Wave Observations

13.2.3 Observed Regional Anisotropy

13.3 FORWARD MODELING

13.3.1 Geodynamic Models

13.3.2 Mineralogical Constraints

Bridgmanite

Post‐perovskite

Ferropericlase

Other Phases

13.4 JOINT GEODYNAMIC–SEISMIC MODELING

13.4.1 Recent Developments

13.4.2 Example Case: Comparing a Model to Seismic Observations

Geodynamic and Texture Modeling

Seismic Modeling

Synthetic Analysis

13.5 LIMITATIONS, ADVANCES, AND THE WAY FORWARD. 13.5.1 The Inverse Problem

13.5.2 Outlook

13.6 ACKNOWLEDGMENTS

REFERENCES

14 Seismic Imaging of Deep Mantle Plumes

ABSTRACT

14.1 INTRODUCTION

14.2 PHYSICAL MODELS OF DEEP MANTLE PLUMES

14.3 TRAVELTIME ANALYSIS

14.3.1 Expected Traveltime Delays

14.3.2 Synthetic Tomography of Deep Mantle Plumes

14.4 UNDULATIONS OF THE 410‐KM AND 660‐KM PHASE TRANSITIONS

14.5 DIFFRACTION AND SCATTERING EFFECTS

14.6 CONCLUDING REMARKS

ACKNOWLEDGMENTS

REFERENCES

15 Observational Estimates of Dynamic Topography Through Space and Time

ABSTRACT

15.1 INTRODUCTION

15.2 CONVECTIVE REGIMES AND THEIR SURFACE EXPRESSION

15.2.1 Thermal Convection of the Mantle

15.2.2 Dynamic Topography: A Definition

15.2.3 Simple Convection Simulations

15.3 EARLY OBSERVATIONAL CONSTRAINTS ON LARGE‐SCALE MANTLE FLOW AND THEIR ROLE IN PAST AND PRESENT GEODYNAMIC MODELING

15.4 ESTIMATING PRESENT‐DAY DYNAMIC TOPOGRAPHY

15.4.1 Oceanic Residual Depth Anomalies

15.4.2 Continental Residual Topography

15.5 OBSERVATIONAL ESTIMATES OF TIME‐EVOLVING DYNAMIC TOPOGRAPHY

15.5.1 Satellite Observations

15.5.2 Sea‐Level Markers

15.5.3 Sedimentary Flux and Stratal Architecture of Basins

15.5.4 Peneplanation and Palaeosurfaces

15.5.5 Landscape Denudation and Thermochronology

15.5.6 Drainage Analysis

15.5.7 Paleoaltimetry

15.5.8 Bathymetric Indicators

15.6 FRONTIERS AND OUTSTANDING CHALLENGES

15.6.1 Continental Residual Topography

15.6.2 Integrated Landscape Evolution Analysis

15.6.3 Spectral Properties of Dynamic Topography

15.6.4 Flow Regime in the Asthenosphere

15.6.5 Numerical Convection Models and Rheology of the Upper Mantle

15.7 SUMMARY

ACKNOWLEDGMENTS

REFERENCES

16 Connecting the Deep Earth and the Atmosphere

ABSTRACT

16.1 INTRODUCTION

16.2 OBSERVED LINKS BETWEEN DEEP EARTH AND SURFACE VOLCANISM

16.3 PLUME ASCENT SCENARIOS

16.4 VOLCANISM AND ENVIRONMENTAL EFFECTS ON VARIOUS TIMESCALES

16.4.1 Kimberlites

16.4.2 Large Igneous Provinces and Global Changes

16.5 LIPs AND PALEOGEOGRAPHY: LONG‐TERM EFFECTS

16.5.1 Plate Tectonic Configurations and Their Modifications by LIPs

16.5.2 Paleoclimate and Atmospheric CO2

16.5.3 Paleolatitude of LIP Emplacement

16.5.4 GEOCARBSULF: Proxy‐Model CO2 Mismatches

16.6 CONCLUDING REMARKS AND CHALLENGES

ACKNOWLEDGMENTS

REFERENCES

APPENDIX 16.1

17 Mercury, Moon, Mars: Surface Expressions of Mantle Convection and Interior Evolution of Stagnant‐Lid Bodies

ABSTRACT

17.1 INTRODUCTION

17.2 MAGMA OCEAN SOLIDIFICATION AND ONSET OF SOLID‐STATE MANTLE CONVECTION

17.2.1 Late Onset of Mantle Convection and Global Overturn

17.2.2 Early Onset of Mantle Convection and Progressive Mixing

17.3 CRUSTAL MANIFESTATIONS

17.3.1 Primary Crusts

17.3.2 Volume and Time of Emplacement of the Secondary Crust

17.4 IMPACTS

17.4.1 Basin Formation

17.4.2 Impact‐Induced Melting

17.4.3 Impact‐Related Effects on Global Mantle Dynamics

17.4.4 Local Signatures of Impact‐Related Effects

17.5 MANTLE COOLING AND MAGNETIC FIELD GENERATION

17.5.1 Mercury’s Present‐Day and Early Magnetic Field

17.5.2 Mars’s Early Magnetic Field

17.5.3 The Long‐Lived Lunar Magnetic Field

17.6 ADDITIONAL SURFICIAL MANIFESTATION

17.6.1 Global Contraction and Expansion

17.6.2 Heat Flux and Elastic Lithosphere Thickness

17.7 SUMMARY AND OUTLOOK

ACKNOWLEDGMENTS

REFERENCES

NOTE

INDEX

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Hauke Marquardt Maxim Ballmer Sanne Cottaar Jasper Konter

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Figure 2.5 Summary of the various textures types observed in post‐perovskite structured compounds over a range of pressure and temperature conditions. Textures are represented as equal area, upper hemisphere projection, inverse pole figures of the compression direction. Scale bar is in multiples of random distribution.

Evidence for (100) or and/ or {110}〈10〉 comes from theoretical calculations and two early DAC studies. First‐principles metadynamics and energetics of stacking faults predicted slip on {110}〈10〉 during the phase transformation from Brg to pPv (Oganov et al., 2005). Shortly thereafter, room temperature radial diffraction DAC experiments on MgGeO3 pPv and MgSiO3 pPv found textures characterized by (100) planes at high angles to compression (Figure 2.5b, c). Polycrystal plasticity modeling showed that these texture could be explained by slip on {110}〈10〉 and (100) planes (Merkel et al., 2006, 2007). It is important to note that both Merkel et al. (2006) and Merkel et al. (2007) converted to the pPv phase directly from the enstatite phase, and no change in texture was observed upon further pressure increase. Subsequent studies on MgGeO3 pPv in the DAC using axial diffraction geometry (Okada et al., 2010) and radial diffraction geometry (Miyagi et al., 2011) found that alignment of (100) planes at high angles to compression resulted from the phase transformation from an enstatite starting material (Figure 2.5d). Further compression showed that the initial (100) transformation texture shifted to (001) (Figure 2.5e) upon deformation consistent with dominant slip on (001)[100] (Table 1; Miyagi et al., 2011; Okada et al., 2010).

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