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Localized polymorphic phase transformations in high‐pressure faults and applications to the physical mechanism of deep earthquakes

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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Experimental Rock Deformation — The Brittle Field

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Rheologies of H20 Ices Ih, II, And III at High Pressures: A Progress Report

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Stability Relations of Silicate Spinels, Ilmenites, and Perovskites

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The earth, its origin, history and physical constitution

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Kinetics of the olivine→spinel transition: Implications to deep-focus earthquake genesis

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Modern physics for the engineer

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Phase transformations and the constitution of the mantle

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Source parameters of intermediate and deep focus earthquakes in the Tonga arc

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Phase transformations, earthquakes and the descending lithosphere

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Thermodynamic constraints on phase changes as earthquake source mechanisms in subduction zones

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Earthquakes resulting from metastable phase transitions

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Temperature and potential temperature beneath island arcs

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Kinetics of high-pressure phase transformations: Implications to the evolution of the olivine → spinel transition in the downgoing lithosphere and its consequences on the dynamics of the mantle

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High-temperature creep of Mt. Burnet Dunite

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Reaction-enhanced ductility: The role of solid-solid univariant reactions in deformation of the crust and mantle

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On the nomenclature of mode of failure transitions in rocks

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X.—Note on Fracture

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Phase transformation under stress and volume transfer creep

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Thermal regime of a downgoing slab and new global tectonics

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The mechanism at the focus of deep earthquakes

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Temperature field and geophysical effects of a downgoing slab

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Elastic constants of the central force model for cubic structures: Polycrystalline aggregates and instabilities

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Structure of the olivine-spinel phase boundary in the descending lithosphere

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Seismic moments of earthquakes beneath island arcs, phase changes, and subduction velocities

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Temporal variation of the activity of intermediate and deep focus earthquakes

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Focal mechanisms and seismic energy release of deep and intermediate earthquakes in the Tonga‐Kermadec Region and their bearing on the depth extent of mantle flow

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Tectonic stresses in the lithosphere: Constraints provided by the experimental deformation of rocks

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Creep mechanism in Mg2GeO4: Effects of a phase transition

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On transformation plasticity

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Experimental deformation of polycrystalline H2O ice at high pressure and low temperature: Preliminary results

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Slab penetration into the lower mantle

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Deformation of clinopyroxenite: Evidence for a transition in flow mechanisms and semibrittle behavior

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The depths of the deepest deep earthquakes

inferredcites →https://doi.org/10.1029/jb091ib03p03573openalex-snapshot

Slab penetration into the lower mantle beneath the Mariana and other island arcs of the northwest Pacific

inferredcites →https://doi.org/10.1029/jb092ib13p13927openalex-snapshot

Spatial patterns of aftershocks of deep focus earthquakes

inferredcites →https://doi.org/10.1029/jb092ib13p13944openalex-snapshot

Aftershocks and temporal clustering of deep earthquakes

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The thermodynamic theory of nonhydrostatically stressed solids

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Experimental deformation of serpentinite and its tectonic implications

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Deep earthquake zones, anomalous structures in the upper mantle, and the lithosphere

inferredcites →https://doi.org/10.1029/rg009i001p00103openalex-snapshot

Distribution of stresses in the descending lithosphere from a global survey of focal‐mechanism solutions of mantle earthquakes

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Nonhydrostatic thermodynamics and its geologic applications

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Phase transitions and mantle discontinuities

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Rheology of the lithosphere

inferredcites →https://doi.org/10.1038/307505a0openalex-snapshot

Deep seismicity and modes of deformation in Tonga subduction zone

inferredcites →https://doi.org/10.1038/308505a0openalex-snapshot

The olivine → spinel transformation and the rheology of subducting lithosphere

inferredcites →https://doi.org/10.1086/624468openalex-snapshot

Shearing Phenomena at High Pressure of Possible Importance for Geology

inferredcites →https://doi.org/10.1086/624495openalex-snapshot

Deep-Focus Earthquakes and Their Geological Significance

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The strains produced by precipitation in alloys

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The determination of the elastic field of an ellipsoidal inclusion, and related problems

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Non-hydrostatic thermodynamics of chemical systems

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On the Arrival of Earthquake Waves at the Antipodes, and on the Measurement of the Focal Depth of an Earthquake.

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The Times of Transmission and Focal Depths of Large Earthquakes.

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Effect of Pressure on Stress-Strain Properties of Materials

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Tectonic Implications of Serpentinite Weakening

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Role of Phase Transitions in a Dynamic Mantle

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Systematic analysis of deep seismicity: 200 centroid-moment tensor solutions for earthquakes between 1977 and 1980

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Focal Mechanisms of Deep and Shallow Earthquakes in the Tonga-Kermadec Region and the Tectonics of Island Arcs

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Thermal Structure of Island Arcs

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Chapter 12: Mechanism of Seismic Faulting

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Chapter 13: Observations on Fracture and a Hypothesis of Earthquakes

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Phase Transformations in Metals and Alloys

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Chapter 2. EXPERIMENTAL STUDIES OF AMPHIBOLE STABILITY

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Motion of the surface of the earth in the compressional phase of a deep-focus earthquake, and the effects of a layered crust

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Earthquakes and faults

inferredcites →https://doi.org/10.1785/bssa0530050893openalex-snapshot

Source wave forms of three earthquakes

inferredcites →https://doi.org/10.1785/bssa0570010009openalex-snapshot

On the occurrence of volume change at the earthquake source

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Thermodynamics of solids under non-hydrostatic stress with geologic applications

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The mechanism of the earthquakes

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POLYMORPHIC TRANSITIONS AND GEOLOGICAL PHENOMENA

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Generation of Elastic Shocks Accompanied with a Phase Change on NH4F

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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Global and along‐strike variations of source duration and scaling for intermediate‐depth and deep‐focus earthquakes

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Dehydration‐induced instabilities at intermediate depths in subduction zones

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Experimental studies on elastic and rheological properties of amphibolites at high pressure and high temperature

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Analytic Solution to the Moment Tensor—Anisotropy Inverse Problem

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Space-time distribution of deep seismic deformation in Tonga

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High-pressure deformation of calcite marble and its transformation to aragonite under non-hydrostatic conditions

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Experimental dynamic metamorphism of mineral single crystals

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Global large deep-focus earthquakes: Source process and cascading failure of shear instability as a unified physical mechanism

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Elasticity of single-crystal olivine at high pressures and temperatures

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Laboratory earthquakes triggered during eclogitization of lawsonite-bearing blueschist

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Experimental evidence for wall-rock pulverization during dynamic rupture at ultra-high pressure conditions

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Coupled strain-induced alpha to omega phase transformation and plastic flow in zirconium under high pressure torsion in a rotational diamond anvil cell

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Upward migration of earthquake hypocenters in Japan, Kurile–Kamchatka and Sunda subduction zones

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Thermal diffusivity and conductivity of olivine, wadsleyite and ringwoodite to 20 GPa and 1373 K

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Simultaneous acoustic emissions monitoring and synchrotron X-ray diffraction at high pressure and temperature: Calibration and application to serpentinite dehydration

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Spatial correlation of deformation and mineral reaction in experimentally deformed plagioclase–olivine aggregates

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Reaction-induced weakening of plagioclase–olivine composites

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Transformational faulting in Mn2GeO4 from olivine to wadsleyite structure: Implications for physical mechanism of deep-focus earthquakes

inferred← citeshttps://doi.org/10.1016/j.xphs.2018.09.015openalex-snapshot

Compression-Induced Polymorphic Transformation in Tablets: Role of Shear Stress and Development of Mitigation Strategies

inferred← citeshttps://doi.org/10.1016/s0012-821x(99)00107-7openalex-snapshot

Numerical tests on the seismic visibility of metastable minerals in subduction zones

inferred← citeshttps://doi.org/10.1016/s0024-4937(01)00037-8openalex-snapshot

Interaction between fluid flow, fracturing and mineral growth during eclogitization, an example from the Sunnfjord area, Western Gneiss Region, Norway

inferred← citeshttps://doi.org/10.1016/s0031-9201(01)00217-5openalex-snapshot

Processes and consequences of deep subduction: introduction

inferred← citeshttps://doi.org/10.1016/s0031-9201(01)00220-5openalex-snapshot

Seismic discontinuities and subduction zones

inferred← citeshttps://doi.org/10.1016/s0031-9201(01)00223-0openalex-snapshot

Rheological structure and deformation of subducted slabs in the mantle transition zone: implications for mantle circulation and deep earthquakes

inferred← citeshttps://doi.org/10.1016/s0031-9201(01)00225-4openalex-snapshot

Seismological constraints on the mechanism of deep earthquakes: temperature dependence of deep earthquake source properties

inferred← citeshttps://doi.org/10.1016/s0031-9201(01)00226-6openalex-snapshot

Experimental constraints on the depth of olivine metastability in subducting lithosphere

inferred← citeshttps://doi.org/10.1016/s0031-9201(97)00031-9openalex-snapshot

Stress fields associated with metastable phase transitions in descending slabs and deep-focus earthquakes

inferred← citeshttps://doi.org/10.1016/s0031-9201(97)00109-xopenalex-snapshot

Fine structure of deep Wadati–Benioff zone in the Izu–Bonin region estimated from S-to-P converted phase

inferred← citeshttps://doi.org/10.1016/s0031-9201(98)00086-7openalex-snapshot

Mechanisms of transformation and deformation in Mg1.8Fe0.2SiO4 olivine and wadsleyite under non-hydrostatic stress

inferred← citeshttps://doi.org/10.1016/s0031-9201(98)00116-2openalex-snapshot

Deep earthquakes beneath the Fiji Basin, SW Pacific: Earth's most intense deep seismicity in stagnant slabs

inferred← citeshttps://doi.org/10.1016/s0040-1951(01)00145-7openalex-snapshot

Shear localization in transformation-induced faulting: first-order similarities to brittle shear failure

inferred← citeshttps://doi.org/10.1016/s0040-1951(96)00291-0openalex-snapshot

Processing of crust in the root of the Caledonian continental collision zone: the role of eclogitization

inferred← citeshttps://doi.org/10.1016/s0065-2687(08)60019-9openalex-snapshot

Aftershocks and Fault-Zone Properties

inferred← citeshttps://doi.org/10.1016/s0074-6142(01)80091-7openalex-snapshot

The Anticrack Mechanism of High-Pressure Faulting: Summary of Experimental Observations and Geophysical Implications

inferred← citeshttps://doi.org/10.1016/s0074-6142(02)80235-2openalex-snapshot

32 Rock failure and earthquakes

inferred← citeshttps://doi.org/10.1016/s0370-1573(98)00088-xopenalex-snapshot

Earthquakes: from chemical alteration to mechanical rupture

inferred← citeshttps://doi.org/10.1017/9781316681473openalex-snapshot

The Mechanics of Earthquakes and Faulting

inferred← citeshttps://doi.org/10.1017/9781316681473.001openalex-snapshot

Preface to the first edition

inferred← citeshttps://doi.org/10.1017/9781316681473.002openalex-snapshot

Preface to the second edition

inferred← citeshttps://doi.org/10.1017/9781316681473.003openalex-snapshot

Preface to the third edition

inferred← citeshttps://doi.org/10.1017/9781316681473.004openalex-snapshot

Brittle fracture of rock

inferred← citeshttps://doi.org/10.1017/9781316681473.005openalex-snapshot

Rock friction

inferred← citeshttps://doi.org/10.1017/9781316681473.006openalex-snapshot

Mechanics of faulting

inferred← citeshttps://doi.org/10.1017/9781316681473.007openalex-snapshot

Mechanics of earthquakes

inferred← citeshttps://doi.org/10.1017/9781316681473.008openalex-snapshot

The seismic cycle

inferred← citeshttps://doi.org/10.1017/9781316681473.009openalex-snapshot

Seismotectonics

inferred← citeshttps://doi.org/10.1017/9781316681473.010openalex-snapshot

Earthquake prediction and hazard analysis

inferred← citeshttps://doi.org/10.1017/9781316681473.011openalex-snapshot

References

inferred← citeshttps://doi.org/10.1017/9781316681473.012openalex-snapshot

Index

inferred← citeshttps://doi.org/10.1017/cbo9780511581397.012openalex-snapshot

Brittle compressive failure of unconfined ice

inferred← citeshttps://doi.org/10.1017/cbo9780511581397.013openalex-snapshot

Brittle compressive failure of confined ice

inferred← citeshttps://doi.org/10.1017/cbo9780511818516.007openalex-snapshot

The seismic cycle

inferred← citeshttps://doi.org/10.1017/cbo9780511818516.009openalex-snapshot

Earthquake prediction and hazard analysis

inferred← citeshttps://doi.org/10.1017/s0022143000007395openalex-snapshot

Ice triaxial deformation and fracture

inferred← citeshttps://doi.org/10.1021/jp061795kopenalex-snapshot

Kinetics of Strain-Induced Structural Changes under High Pressure

inferred← citeshttps://doi.org/10.1029/2000jb900097openalex-snapshot

Aftershocks of the March 9, 1994, Tonga earthquake: The strongest known deep aftershock sequence

inferred← citeshttps://doi.org/10.1029/2000jb900314openalex-snapshot

Do intermediate‐ and deep‐focus earthquakes occur on preexisting weak zones? An examination of the Tonga subduction zone

inferred← citeshttps://doi.org/10.1029/2001gl013810openalex-snapshot

Dynamic phase boundaries of olivine‐wadsleyite in subduction zones in the western Pacific

inferred← citeshttps://doi.org/10.1029/2001jb001129openalex-snapshot

Subduction factory 2. Are intermediate‐depth earthquakes in subducting slabs linked to metamorphic dehydration reactions?

inferred← citeshttps://doi.org/10.1029/2001jb001223openalex-snapshot

The effects of metastable olivine(α) wedge in subducted slabs on theoretical seismic waveforms of deep earthquakes

inferred← citeshttps://doi.org/10.1029/2002gl015003openalex-snapshot

A process for low‐temperature olivine‐spinel transition under quasi‐hydrostatic stress

inferred← citeshttps://doi.org/10.1029/2002gl015441openalex-snapshot

Unbending combined with dehydration embrittlement as a cause for double and triple seismic zones

inferred← citeshttps://doi.org/10.1029/2002jb001948openalex-snapshot

Source characteristics of large deep earthquakes: Constraint on the faulting mechanism at great depths

inferred← citeshttps://doi.org/10.1029/2003jb002762openalex-snapshot

Deep earthquake rupture histories determined by global stacking of broadband P waveforms

inferred← citeshttps://doi.org/10.1029/2003jb002945openalex-snapshot

Plastic faulting: Brittle‐like failure under high confinement

inferred← citeshttps://doi.org/10.1029/2004jb003470openalex-snapshot

Earthquakes and strain in subhorizontal slabs

inferred← citeshttps://doi.org/10.1029/2005jb004001openalex-snapshot

Measurement of differential rupture durations as constraints on the source finiteness of deep‐focus earthquakes

inferred← citeshttps://doi.org/10.1029/2006jb004677openalex-snapshot

Earthquake mechanics and deformation in the Tonga‐Kermadec subduction zone from fault plane orientations of intermediate‐ and deep‐focus earthquakes

inferred← citeshttps://doi.org/10.1029/2011jb008730openalex-snapshot

Dehydration‐induced damage and deformation in gypsum and implications for subduction zone processes

inferred← citeshttps://doi.org/10.1029/2018gc007489openalex-snapshot

Source Complexity of the 2015 Mw 7.9 Bonin Earthquake

inferred← citeshttps://doi.org/10.1029/2018gl080997openalex-snapshot

Complex and Diverse Rupture Processes of the 2018 M w 8.2 and M w 7.9 Tonga‐Fiji Deep Earthquakes

inferred← citeshttps://doi.org/10.1029/2019gl085589openalex-snapshot

The Preseismic and Postseismic Phases of the 700‐km Deep M7.9 Bonin Islands Earthquake, Japan

inferred← citeshttps://doi.org/10.1029/2019gl086055openalex-snapshot

Stress Drop Variation of Deep‐Focus Earthquakes Based on Empirical Green's Functions

inferred← citeshttps://doi.org/10.1029/2019gl086125openalex-snapshot

High Rates of Deep Earthquake Dynamic Triggering in the Thermal Halos of Subducting Slabs

inferred← citeshttps://doi.org/10.1029/2020gl090744openalex-snapshot

Deep Ductile Shear Zone Facilitates Near‐Orthogonal Strike‐Slip Faulting in a Thin Brittle Lithosphere

inferred← citeshttps://doi.org/10.1029/2021gl093111openalex-snapshot

Lower Mantle Seismicity Following the 2015 Mw 7.9 Bonin Islands Deep‐Focus Earthquake

inferred← citeshttps://doi.org/10.1029/2021jb023658openalex-snapshot

Imbalanced Moment Release Within Subducting Plates During Initial Bending and Unbending

inferred← citeshttps://doi.org/10.1029/2022jb025109openalex-snapshot

Stress Drops of Intermediate‐Depth and Deep Earthquakes in the Tonga Slab

inferred← citeshttps://doi.org/10.1029/2022je007364openalex-snapshot

Stresses in the Lunar Interior: Insights From Slip Directions in the A01 Deep Moonquake Nest

inferred← citeshttps://doi.org/10.1029/2024ea003617openalex-snapshot

Deep‐Focus Earthquake Mechanisms at the Subducting Nazca Plate (Peru‐Brazil Border): Cold Slab Behavior in a Warm Plate

inferred← citeshttps://doi.org/10.1029/2024gl111281openalex-snapshot

Severe Strain‐Induced Olivine‐Ringwoodite Transformation at Room Temperature: Key to Enigmas of Deep‐Focus Earthquake

inferred← citeshttps://doi.org/10.1029/2024jb028846openalex-snapshot

Rapid Ductile Strain Localization Due To Thermal Runaway

inferred← citeshttps://doi.org/10.1029/2024jb030557openalex-snapshot

Numerical Investigation Into Mechanical Behavior of Metastable Olivine During Phase Transformation: Implications for Deep‐Focus Earthquakes

inferred← citeshttps://doi.org/10.1029/2025av001701openalex-snapshot

Dual Mechanism Transition Controls Rupture Development of Large Deep Earthquakes

inferred← citeshttps://doi.org/10.1029/2025gl121541openalex-snapshot

Decomposing Earthquake Moment Tensors Using P‐Wave First Motion: Insights Into Global Events With Significant Non‐Double‐Couple Components

inferred← citeshttps://doi.org/10.1029/2025jb031240openalex-snapshot

Transient Propagation of Ductile Ruptures by Thermal Runaway

inferred← citeshttps://doi.org/10.1029/90jb01937openalex-snapshot

Faulting associated with the olivine to spinel transformation in Mg2GeO4 and its implications for deep‐focus earthquakes

inferred← citeshttps://doi.org/10.1029/91gl01081openalex-snapshot

A simple explanation for the depth distribution of deep earthquakes

inferred← citeshttps://doi.org/10.1029/92jb02174openalex-snapshot

Some observations on the effects of shear stress on a polymorphic transformation in perovskite‐structured lead‐zirconate‐titanate ceramic

inferred← citeshttps://doi.org/10.1029/93jb01564openalex-snapshot

Flow of ices in the ammonia‐water system

inferred← citeshttps://doi.org/10.1029/93jb01614openalex-snapshot

Shear‐promoted phase transitions in Fe2SiO4 and Mg2SiO4 and the mechanism of deep earthquakes

inferred← citeshttps://doi.org/10.1029/93jb02873openalex-snapshot

The brittle‐plastic transition in experimentally deformed quartz aggregates

inferred← citeshttps://doi.org/10.1029/94gl01083openalex-snapshot

Two types of deep seismicity in subducting slabs

inferred← citeshttps://doi.org/10.1029/94jb00038openalex-snapshot

Isolated deep earthquakes and the fate of subduction in the mantle

inferred← citeshttps://doi.org/10.1029/95rg00178openalex-snapshot

Rock deformation: Ductile and brittle

inferred← citeshttps://doi.org/10.1029/95rg00353openalex-snapshot

Interslab earthquakes and phase changes in subducting lithosphere

inferred← citeshttps://doi.org/10.1029/96gl03023openalex-snapshot

High‐pressure phase transition in Al(OH)3: Raman and X‐ray observations

inferred← citeshttps://doi.org/10.1029/96jb03221openalex-snapshot

A constitutive model for olivine‐spinel aggregates and its application to deep earthquake nucleation

inferred← citeshttps://doi.org/10.1029/96rg01050openalex-snapshot

Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere

inferred← citeshttps://doi.org/10.1029/97gl01245openalex-snapshot

The Complex Rupture Process of the 1996 Deep Flores, Indonesia Earthquake (Mw 7.9) from teleseismic P‐waves

inferred← citeshttps://doi.org/10.1029/97gl03277openalex-snapshot

Seismological evidence for the existence of anisotropic zone in the metastable wedge inside the subducting Izu‐Bonin Slab

inferred← citeshttps://doi.org/10.1029/98gl02567openalex-snapshot

Comment on “Seismological evidence for the existence of anisotropic zone in the metastable wedge inside the subducting Izu‐Bonin Slab” by Takashi Iidaka and Kazushige Obara

inferred← citeshttps://doi.org/10.1029/98jb00595openalex-snapshot

Topography on the 410‐km seismic velocity discontinuity near subduction zones from stacking of sS, sP, and pP precursors

inferred← citeshttps://doi.org/10.1029/98jb01517openalex-snapshot

Modeling the Tonga slab: Can travel time data resolve a metastable olivine wedge?

inferred← citeshttps://doi.org/10.1029/98jb02135openalex-snapshot

Time functions of deep earthquakes from broadband and short‐period stacks

inferred← citeshttps://doi.org/10.1029/98rg00716openalex-snapshot

Non‐double‐couple earthquakes 1. Theory

inferred← citeshttps://doi.org/10.1029/gl015i010p01081openalex-snapshot

Rheological control of Wadati‐Benioff zone seismicity

inferred← citeshttps://doi.org/10.1029/gm056p0127openalex-snapshot

Brittle/ductile and plastic/cataclastic transitions in experimentally deformed and metamorphosed amphibolite

inferred← citeshttps://doi.org/10.1029/gm096p0001openalex-snapshot

Thermo-Mechanical Evolution of Oceanic Lithosphere: Implications for the Subduction Process and Deep Earthquakes

inferred← citeshttps://doi.org/10.1029/gm096p0223openalex-snapshot

Plate Structure and the Origin of Double Seismic Zones

inferred← citeshttps://doi.org/10.1029/gm096p0357openalex-snapshot

Characteristics of Multiple Ruptures During Large Deep-Focus Earthquakes

inferred← citeshttps://doi.org/10.1029/gm101p0483openalex-snapshot

Yield strength, slip systems and deformation induced phase transition of San Carlos olivine up to the transition zone pressure at room temperature

inferred← citeshttps://doi.org/10.1029/jb092ib13p13777openalex-snapshot

Kiyoo Wadati and early research on deep focus earthquakes: Introduction to Special Section on Deep and Intermediate Focus Earthquakes

inferred← citeshttps://doi.org/10.1029/jb093ib07p07625openalex-snapshot

Friction of ice

inferred← citeshttps://doi.org/10.1038/338703a0openalex-snapshot

Mechanisms of phase changes

inferred← citeshttps://doi.org/10.1038/339616a0openalex-snapshot

Acoustic emissions and shear instabilities during phase transformations in Si and Ge at ultrahigh pressures

inferred← citeshttps://doi.org/10.1038/341687a0openalex-snapshot

New rumbles on deep sources

inferred← citeshttps://doi.org/10.1038/341733a0openalex-snapshot

A new self-organizing mechanism for deep-focus earthquakes

inferred← citeshttps://doi.org/10.1038/347620a0openalex-snapshot

Metastable phases confirmed

inferred← citeshttps://doi.org/10.1038/348628a0openalex-snapshot

Mechanism of the γ–β phase transformation of Mg2SiO4 at high temperature and pressure

inferred← citeshttps://doi.org/10.1038/348720a0openalex-snapshot

Anticrack-associated faulting at very high pressure in natural olivine

inferred← citeshttps://doi.org/10.1038/351050a0openalex-snapshot

Insignificant isotropic component in the moment tensor of deep earthquakes

inferred← citeshttps://doi.org/10.1038/351140a0openalex-snapshot

Aseismicity in the lower mantle by superplasticity of the descending slab

inferred← citeshttps://doi.org/10.1038/352520a0openalex-snapshot

Fast rise times and the physical mechanism of deep earthquakes

inferred← citeshttps://doi.org/10.1038/353252a0openalex-snapshot

Relationship of deep seismicity to the thermal structure of subducted lithosphere

inferred← citeshttps://doi.org/10.1038/356593a0openalex-snapshot

Seismological evidence for metastable olivine inside a subducting slab

inferred← citeshttps://doi.org/10.1038/358574a0openalex-snapshot

An earthquake mechanism based on rapid sealing of faults

inferred← citeshttps://doi.org/10.1038/361626a0openalex-snapshot

Deformation of a weak subducted slab and variation of seismicity with depth

inferred← citeshttps://doi.org/10.1038/364790a0openalex-snapshot

Evidence for transformational faulting from a deep double seismic zone in Tonga

inferred← citeshttps://doi.org/10.1038/365045a0openalex-snapshot

The depth dependence of earthquake duration and implications for rupture mechanisms

inferred← citeshttps://doi.org/10.1038/368100a0openalex-snapshot

A break in the deep

inferred← citeshttps://doi.org/10.1038/372540a0openalex-snapshot

A deep earthquake aftershock sequence and implications for the rupture mechanism of deep earthquakes

inferred← citeshttps://doi.org/10.1038/374249a0openalex-snapshot

Geodetic observations of very rapid convergence and back-arc extension at the Tonga arc

inferred← citeshttps://doi.org/10.1038/384153a0openalex-snapshot

Effect of slab temperature on deep-earthquake aftershock productivity and magnitude–frequency relations

inferred← citeshttps://doi.org/10.1038/414893aopenalex-snapshot

Striped iron zoning of olivine induced by dislocation creep in deformed peridotites

inferred← citeshttps://doi.org/10.1038/s41467-022-33802-yopenalex-snapshot

Resolving puzzles of the phase-transformation-based mechanism of the strong deep-focus earthquake

inferred← citeshttps://doi.org/10.1038/s41561-018-0188-3openalex-snapshot

Deep earthquakes in subducting slabs hosted in highly anisotropic rock fabric

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