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The interface-scale mechanism of reaction-induced fracturing during serpentinization

https://doi.org/10.1130/g33390.1
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What this work says

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

inferredcites →https://doi.org/10.1007/bf00311845openalex-snapshot
Dislocation substructure of mantle-derived olivine as revealed by selective chemical etching and transmission electron microscopy
inferredcites →https://doi.org/10.1007/s00410-008-0324-yopenalex-snapshot
Reaction induced fracturing during replacement processes
inferredcites →https://doi.org/10.1016/0016-7037(78)90245-4openalex-snapshot
Changes in surface area and morphology and the mechanism of forsterite dissolution
inferredcites →https://doi.org/10.1016/0031-9201(85)90128-1openalex-snapshot
Ductile-brittle transition investigated by micro-indentation: results for quartz and olivine
inferredcites →https://doi.org/10.1016/0040-1951(85)90225-2openalex-snapshot
Rate of serpentinization in seafloor environments
inferredcites →https://doi.org/10.1016/0098-3004(92)90029-qopenalex-snapshot
SUPCRT92: A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1 to 5000 bar and 0 to 1000°C
inferredcites →https://doi.org/10.1016/j.chemgeo.2011.02.021openalex-snapshot
Influence of amorphous silica layer formation on the dissolution rate of olivine at 90°C and elevated pCO2
inferredcites →https://doi.org/10.1016/j.chemgeo.2011.08.007openalex-snapshot
Progress of hydration reactions in olivine–H2O and orthopyroxenite–H2O systems at 250 °C and vapor-saturated pressure
inferredcites →https://doi.org/10.1016/j.chemgeo.2011.12.002openalex-snapshot
Unifying natural and laboratory chemical weathering with interfacial dissolution–reprecipitation: A study based on the nanometer-scale chemistry of fluid–silicate interfaces
inferredcites →https://doi.org/10.1016/j.engfailanal.2009.04.004openalex-snapshot
Numerical investigation on stress concentration of corrosion pit
inferredcites →https://doi.org/10.1016/j.epsl.2004.02.012openalex-snapshot
The fate of B, Cl and Li in the subducted oceanic mantle and in the antigorite breakdown fluids
inferredcites →https://doi.org/10.1016/j.epsl.2006.11.015openalex-snapshot
Diffusion in solid-Earth systems
inferredcites →https://doi.org/10.1016/j.epsl.2007.11.060openalex-snapshot
Reaction-assisted hierarchical fracturing during serpentinization
inferredcites →https://doi.org/10.1016/j.epsl.2008.08.035openalex-snapshot
Controls on rock weathering rates by reaction-induced hierarchical fracturing
inferredcites →https://doi.org/10.1016/j.epsl.2010.01.016openalex-snapshot
A simple model of reaction-induced cracking applied to serpentinization and carbonation of peridotite
inferredcites →https://doi.org/10.1016/j.gca.2009.08.021openalex-snapshot
Iron partitioning and hydrogen generation during serpentinization of abyssal peridotites from 15°N on the Mid-Atlantic Ridge
inferredcites →https://doi.org/10.1016/s0065-2156(08)70121-2openalex-snapshot
The Mathematical Theory of Equilibrium Cracks in Brittle Fracture
inferredcites →https://doi.org/10.1017/s0016756800011389openalex-snapshot
Fluid supersaturation and crystallization in porous media
inferredcites →https://doi.org/10.1021/es9038193openalex-snapshot
Effect of Secondary Phase Formation on the Carbonation of Olivine
inferredcites →https://doi.org/10.1029/2006gc001373openalex-snapshot
Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites
inferredcites →https://doi.org/10.1029/2011jb008842openalex-snapshot
Serpentinization of oceanic peridotites: 2. Kinetics and processes of San Carlos olivine hydrothermal alteration
inferredcites →https://doi.org/10.1029/jb074i025p05961openalex-snapshot
Elastic moduli, pressure derivatives, and temperature derivatives of single-crystal olivine and single-crystal forsterite
inferredcites →https://doi.org/10.1073/pnas.0405289101openalex-snapshot
H 2 -rich fluids from serpentinization: Geochemical and biotic implications
inferredcites →https://doi.org/10.1073/pnas.0507777102openalex-snapshot
Mechanisms of classical crystal growth theory explain quartz and silicate dissolution behavior
inferredcites →https://doi.org/10.1093/petrology/egp049openalex-snapshot
Serpentine Mineral Replacements of Natural Olivine and their Seismic Implications: Oceanic Lizardite versus Subduction-Related Antigorite
inferredcites →https://doi.org/10.1103/physreve.79.046109openalex-snapshot
Drying patterns: Sensitivity to residual stresses
inferredcites →https://doi.org/10.1127/0935-1221/2004/0016-0731openalex-snapshot
Oriented, non-topotactic olivine serpentine replacement in mesh-textured, serpentinized peridotites
inferredcites →https://doi.org/10.1127/ejm/10/6/1341openalex-snapshot
Mesh textures and bastites in the Elba retrograde serpentinites
inferredcites →https://doi.org/10.1130/0091-7613(2001)029<1023:sosspi>2.0.co;2openalex-snapshot
Strength of slightly serpentinized peridotites: Implications for the tectonics of oceanic lithosphere
inferredcites →https://doi.org/10.1146/annurev-earth-092010-152509openalex-snapshot
Rates and Mechanisms of Mineral Carbonation in Peridotite: Natural Processes and Recipes for Enhanced, in situ CO 2 Capture and Storage
inferredcites →https://doi.org/10.2138/am.2011.3779openalex-snapshot
Experimental investigations into the silicification of olivine: Implications for the reaction mechanism and acid neutralization
inferredcites →https://doi.org/10.2138/rmg.2009.70.3openalex-snapshot
Mineral Replacement Reactions
inferredcites →https://doi.org/10.2747/0020-6814.46.6.479openalex-snapshot
The Serpentinite Multisystem Revisited: Chrysotile Is Metastable
inferredcites →https://doi.org/10.5006/1.3577891openalex-snapshot
Prediction of Fatigue Crack Initiation Life Based on Pit Growth

What points at this work

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

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Lithology's Influence on Biogenic Phosphatization on Oceanic Islands, Equatorial Atlantic, Brazil
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Volumetric Response and Permeability Evolution During Carbonation of Crushed Peridotite Under Controlled Stress-P-T Conditions
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Reaction‐driven fracturing of porous rock
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Dissolution–precipitation processes governing the carbonation and silicification of the serpentinite sole of the New Caledonia ophiolite
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Grain boundaries as microreactors during reactive fluid flow: experimental dolomitization of a calcite marble
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The roles of fluid transport and surface reaction in reaction-induced fracturing, with implications for the development of mesh textures in serpentinites
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Reactive fluid flow guided by grain-scale equilibrium reactions during eclogitization of dry crustal rocks
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Halogens in serpentinised-troctolites from the Atlantis Massif: implications for alteration and global volatile cycling
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Factors controlling reaction pathways during fluid–rock interactions
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Precipitation of Calcite Veins in Serpentinized Harzburgite at Tianxiu Hydrothermal Field on Carlsberg Ridge (3.67°N), Northwest Indian Ocean: Implications for Fluid Circulation
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Achieving complete reaction while the solid volume increases: A numerical model applied to serpentinisation
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Seismic faults triggered early stage serpentinization of peridotites from the Samail Ophiolite, Oman
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Nanostructure of serpentinisation products: Importance for water transport and low-temperature alteration
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Weathering-driven porosity generation in altered oceanic peridotites
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The role of sulfate in the hydrothermal replacement of aragonite single crystals by calcite
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Massive Mg-rich fluid release across the brucite + serpentine reaction in subduction zones
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Exhumation-induced residual stress in undeformed ultra-high-pressure metamorphic rock
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The serpentinized oceanic mantle: A potentially substantial volatile sink
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Outer-rise serpentinization water flux: a fault-localized mechanism with nonlinear controls
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Garnets within geode-like serpentinite veins: Implications for element transport, hydrogen production and life-supporting environment formation
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Formation of iddingsite veins in the martian crust by centripetal replacement of olivine: Evidence from the nakhlite meteorite Lafayette
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Effect of pH and temperature on olivine dissolution anisotropy
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Impact of coating structure on the rates of coupled dissolution-precipitation reactions
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Spatiotemporal monitoring of serpentinization in peridotite: mineral replacement, volume change and hydrogen production
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Serpentinization-driven extension in the Ronda mantle slab (Betic Cordillera, S. Spain)
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Short lifespans of serpentinization in the rocky core of Enceladus: Implications for hydrogen production
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Evaluation and site selection for carbon storage via shallow CO2 injection into serpentinite in British Columbia, Canada
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Computer simulation of reaction and transport of core-scale serpentinization of Fe-bearing olivine and evolution of geological hydrogen
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Volumetric response and permeability evolution during carbonation of crushed peridotite under controlled stress-pressure-temperature conditions
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Experimental study of the effects of solute transport on reaction paths during incipient serpentinization
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In-situ oxygen isotope analyses in serpentine minerals: Constraints on serpentinization during tectonic exhumation at slow- and ultraslow-spreading ridges
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Evidence for multiple stages of serpentinization from the mantle through the crust in the Redwood City Serpentinite mélange along the San Andreas Fault in California
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Mineralogical and geochemical study of serpentinized peridotites from the North-Western Pyrenees: New insights on serpentinization along magma-poor continental passive margins
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Iron oxidation and porosity generation in serpentinized abyssal peridotite
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Serpentinization and its implications for ultramafic-hosted sulfide mineralization: A case study at the Tianzuo hydrothermal field, 63.5°E, Southwest Indian Ridge
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Textural and chemical evolution during dedolomitization: A case study of the Benassal Formation, Maestrat Basin, Spain
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How bedding-parallel fractures affect fluid activity in a relatively closed lacustrine shales system: Evidence from calcite veins
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Multi-stage vein formation and diagenetic modification in the first member of the Maokou Formation in the Middle Permian, Sichuan Basin, SW China: implications for the modification of limestone–marl alternations reservoirs
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Crack geometry of serpentinized peridotites inferred from onboard ultrasonic data from the Oman Drilling Project
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Formation of Strontianite and Witherite Cohesive Layers on Calcite Surfaces for Building Stone Conservation
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Reaction-Induced Fracturing of Porous Carbonate Rocks during Volume-Increasing Replacement by Witherite
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How Pre-existing Porosity Networks Affect the Development of Mineral Transformations?
inferred← citeshttps://doi.org/10.1021/acs.chemrev.5c00716openalex-snapshot
Earth as a Reactor: Carbon Mineralization Geochemistry in the Context of Emerging Subsurface Energy and Resource Technologies
inferred← citeshttps://doi.org/10.1021/acs.energyfuels.6c00873openalex-snapshot
Stimulated Serpentinization for Geologic Hydrogen: A Review of Experimental, Modeling, and Field Studies
inferred← citeshttps://doi.org/10.1021/acs.energyfuels.8b01711openalex-snapshot
Gypsum-Crystallization-Induced Fracturing during Shale–Fluid Reactions and Application for Shale Stimulation
inferred← citeshttps://doi.org/10.1021/acs.estlett.9b00301openalex-snapshot
Quantitative Review of Olivine Carbonation Kinetics: Reactivity Trends, Mechanistic Insights, and Research Frontiers
inferred← citeshttps://doi.org/10.1029/2017jb014900openalex-snapshot
Smoke Without Fire: How Long Can Thermal Cracking Sustain Hydrothermal Circulation in the Absence of Magmatic Heat?
inferred← citeshttps://doi.org/10.1029/2017jb015214openalex-snapshot
A Poroelastic Model of Serpentinization: Exploring the Interplay Between Rheology, Surface Energy, Reaction, and Fluid Flow
inferred← citeshttps://doi.org/10.1029/2018gc007851openalex-snapshot
Initiation of Strike‐Slip Faults, Serpentinization, and Methane: The Nootka Fault Zone, the Juan de Fuca‐Explorer Plate Boundary
inferred← citeshttps://doi.org/10.1029/2018gc008092openalex-snapshot
Fault Initiation in Serpentinite
inferred← citeshttps://doi.org/10.1029/2018jb016872openalex-snapshot
Modeling Porosity Evolution Throughout Reaction‐Induced Fracturing in Rocks With Implications for Serpentinization
inferred← citeshttps://doi.org/10.1029/2018jb017008openalex-snapshot
Mixed‐Mode Strain Localization Generated by Hydration Reaction at Crustal Conditions
inferred← citeshttps://doi.org/10.1029/2019gc008492openalex-snapshot
Why Is Crustal Underplating Beneath Many Hot Spot Islands Anisotropic?
inferred← citeshttps://doi.org/10.1029/2019jb018877openalex-snapshot
Measurement of Volume Change and Mass Transfer During Serpentinization: Insights From the Oman Drilling Project
inferred← citeshttps://doi.org/10.1029/2020gc009351openalex-snapshot
2D Hydro‐Mechanical‐Chemical Modeling of (De)hydration Reactions in Deforming Heterogeneous Rock: The Periclase‐Brucite Model Reaction
inferred← citeshttps://doi.org/10.1029/2020gl088472openalex-snapshot
Tracking Subsurface Active Weathering Processes in Serpentinite
inferred← citeshttps://doi.org/10.1029/2020jb020199openalex-snapshot
Brittle Deformation of Carbonated Peridotite—Insights From Listvenites of the Samail Ophiolite (Oman Drilling Project Hole BT1B)
inferred← citeshttps://doi.org/10.1029/2020jb020268openalex-snapshot
Fluid Infiltration Through Oceanic Lower Crust in Response to Reaction‐Induced Fracturing: Insights From Serpentinized Troctolite and Numerical Models
inferred← citeshttps://doi.org/10.1029/2020jb020557openalex-snapshot
Thermo‐Mechanical State of Ultraslow‐Spreading Ridges With a Transient Magma Supply
inferred← citeshttps://doi.org/10.1029/2021gc009711openalex-snapshot
Kinetics and Mechanisms of Acid‐pH Weathering of Pyroxenes
inferred← citeshttps://doi.org/10.1029/2021gc009989openalex-snapshot
Deducing Mineralogy of Serpentinized and Carbonated Ultramafic Rocks Using Physical Properties With Implications for Carbon Sequestration and Subduction Zone Dynamics
inferred← citeshttps://doi.org/10.1029/2021jb021671openalex-snapshot
Hydrostatic Dehydration Fabrics of Antigorite at High Pressure and High Temperature: Implications for Trench Parallel Seismic Anisotropy at Convergent Plate Boundaries
inferred← citeshttps://doi.org/10.1029/2021je006995openalex-snapshot
Theoretical Considerations on the Characteristic Timescales of Hydrogen Generation by Serpentinization Reactions on Enceladus
inferred← citeshttps://doi.org/10.1029/2022gc010498openalex-snapshot
Global Constraints on Intermediate‐Depth Intraslab Stresses From Slab Geometries and Mechanisms of Double Seismic Zone Earthquakes
inferred← citeshttps://doi.org/10.1029/2022jb024621openalex-snapshot
Structural Heterogeneity of the Alaska‐Aleutian Forearc: Implications for Interplate Coupling and Seismogenic Behaviors
inferred← citeshttps://doi.org/10.1029/2022jb024701openalex-snapshot
Forced Subduction Initiation Near Spreading Centers: Effects of Brittle‐Ductile Damage
inferred← citeshttps://doi.org/10.1029/2024gc011581openalex-snapshot
Fluid‐Driven Shear Instabilities in the Subducted Oceanic Mantle at Intermediate Depths: Insights From Western Alps Meta‐Ophiolites
inferred← citeshttps://doi.org/10.1029/2024tc008586openalex-snapshot
The Effect of Brittle‐Ductile Weakening on the Formation of Faulting Patterns at Mid‐Ocean Ridges
inferred← citeshttps://doi.org/10.1029/2025gl119699openalex-snapshot
An Approach to Sustainable Hydrogen Generation From Stimulated Iron‐Rich Ultramafic Rock
inferred← citeshttps://doi.org/10.1029/2025jb032133openalex-snapshot
Slowly Migrating Fracture Swarms in an Actively Serpentinizing Borehole
inferred← citeshttps://doi.org/10.1029/2025jb032776openalex-snapshot
Quantifying Vein Network Permeability in Dehydrated Serpentinites Using Thermodynamics and Generative AI
inferred← citeshttps://doi.org/10.1029/2025jb032881openalex-snapshot
Transient Porosity During Fluid‐Mineral Interaction. Part 1: In Situ 4D Tomography
inferred← citeshttps://doi.org/10.1029/2025jb033125openalex-snapshot
Unraveling Dissolution‐Precipitation Evolution in Basalt During Supercritical CO 2 ‐Water‐Rock (CWR) Interaction: A Mesoscale Mechanical Perspective
inferred← citeshttps://doi.org/10.1029/2025je009278openalex-snapshot
Contrasting Olivine Alteration Scenario in the Deccan Continental Flood Basalt, India: Implications for Mars
inferred← citeshttps://doi.org/10.1029/2025jh000666openalex-snapshot
An AI‐Enabled Data Processing Pipeline for Ingesting Borehole Data in Peridotite Environments
inferred← citeshttps://doi.org/10.1029/2026gc012944openalex-snapshot
Structurally‐Controlled Permeability Evolution and Mineralization in Geothermal Caprocks: The Fenice Capanne Mining District (Southern Tuscany, Italy)
inferred← citeshttps://doi.org/10.1029/2026jb034377openalex-snapshot
Reaction‐Driven Crack Propagation Controlled by Vein Extension in a Dilute Fracture System
inferred← citeshttps://doi.org/10.1038/ncomms15980openalex-snapshot
Dehydration of subducting slow-spread oceanic lithosphere in the Lesser Antilles
inferred← citeshttps://doi.org/10.1038/ncomms16107openalex-snapshot
Effect of water activity on rates of serpentinization of olivine
inferred← citeshttps://doi.org/10.1038/ngeo2865openalex-snapshot
Fluid escape from subduction zones controlled by channel-forming reactive porosity
inferred← citeshttps://doi.org/10.1038/ngeo3009openalex-snapshot
Fluid-driven metamorphism of the continental crust governed by nanoscale fluid flow
inferred← citeshttps://doi.org/10.1038/s41467-026-68507-zopenalex-snapshot
Unveiling the metallogenic continuum of an Archean craton
inferred← citeshttps://doi.org/10.1038/s41467-026-73920-5openalex-snapshot
Controls on natural hydrogen generation during serpentinization of mantle rocks
inferred← citeshttps://doi.org/10.1038/s41570-022-00418-1openalex-snapshot
Molecular-scale mechanisms of CO2 mineralization in nanoscale interfacial water films
inferred← citeshttps://doi.org/10.1038/s41598-020-76813-9openalex-snapshot
Two-stage fluid pathways generated by volume expansion reactions: insights from the replacement of pyrite by chalcopyrite
inferred← citeshttps://doi.org/10.1038/s41598-022-25612-5openalex-snapshot
Carbonation and serpentinization of diopsidite in the Altun Mountains, NW China
inferred← citeshttps://doi.org/10.1038/s41598-023-28970-wopenalex-snapshot
Quantifying microstructures of earth materials using higher-order spatial correlations and deep generative adversarial networks
inferred← citeshttps://doi.org/10.1038/s42004-021-00610-2openalex-snapshot
Direct evidence for metallic mercury causing photo-induced darkening of red cinnabar tempera paints
inferred← citeshttps://doi.org/10.1038/s43017-025-00670-1openalex-snapshot
Natural hydrogen resource accumulation in the continental crust
inferred← citeshttps://doi.org/10.1039/d4va00316kopenalex-snapshot
Porosity and fluid pathway development during cadmium sequestration by calcium carbonate replacement
inferred← citeshttps://doi.org/10.1039/d6ee01230bopenalex-snapshot
Stimulated geologic hydrogen: from mechanistic control to engineered rock transformation
inferred← citeshttps://doi.org/10.1061/9780784412992.099openalex-snapshot
Reaction-Driven Cracking During Mineral Hydration, Carbonation and Oxidation
inferred← citeshttps://doi.org/10.1073/pnas.2110776118openalex-snapshot
Volatile-consuming reactions fracture rocks and self-accelerate fluid flow in the lithosphere
inferred← citeshttps://doi.org/10.1093/gji/ggx341openalex-snapshot
Elastic and electrical properties and permeability of serpentinites from Atlantis Massif, Mid-Atlantic Ridge
inferred← citeshttps://doi.org/10.1093/petrology/egv014openalex-snapshot
Serpentinization and Fluid Pathways in Tectonically Exhumed Peridotites from the Southwest Indian Ridge (62-65 E)
inferred← citeshttps://doi.org/10.1093/petrology/egx071openalex-snapshot
Mid-ocean Ridge Serpentinite in the Puerto Rico Trench: from Seafloor Spreading to Subduction
inferred← citeshttps://doi.org/10.1093/petrology/egy039openalex-snapshot
Al-Zoning of Serpentine Aggregates in Mesh Texture Induced by Metasomatic Replacement Reactions
inferred← citeshttps://doi.org/10.1111/gfl.12169openalex-snapshot
Modeling of hydrogen production by serpentinization in ultramafic‐hosted hydrothermal systems: application to the Rainbow field
inferred← citeshttps://doi.org/10.1111/jmg.12809openalex-snapshot
A Mechanistic Look at the Amphibolitization of Mafic Crust: Insights From the Kråkeneset Gabbro Body, Western Gneiss Region, Norway
inferred← citeshttps://doi.org/10.1111/jmg.70015openalex-snapshot
Interplay Between Mechanical and Petrochemical Models on the Fluid Extraction From Subduction Zones
inferred← citeshttps://doi.org/10.1111/jmg.70028openalex-snapshot
The Contribution of Volume Change in Preserving High‐ P Metastable Assemblages
inferred← citeshttps://doi.org/10.1111/ter.12018openalex-snapshot
Formation of garnet clusters during polyphase metamorphism
inferred← citeshttps://doi.org/10.1127/0935-1221/2013/0025-2346openalex-snapshot
Replacement and ion exchange reactions of scolecite in a high pH aqueous solution
inferred← citeshttps://doi.org/10.1127/ejm/2019/0031-2842openalex-snapshot
The water and fluid-mobile element cycles during serpentinite subduction. A review
inferred← citeshttps://doi.org/10.1130/focus022016.1openalex-snapshot
RESEARCH FOCUS: Serpentinization and the formation of fluid pathways
inferred← citeshttps://doi.org/10.1130/g37349.1openalex-snapshot
Nanoscale constraints on porosity generation and fluid flow during serpentinization
inferred← citeshttps://doi.org/10.1130/g47289.1openalex-snapshot
Quantifying the volume increase and chemical exchange during serpentinization
inferred← citeshttps://doi.org/10.1130/g50493.1openalex-snapshot
High-magnitude stresses induced by mineral-hydration reactions
inferred← citeshttps://doi.org/10.1130/ges02367.1openalex-snapshot
Impact of bending-related faulting and oceanic-plate topography on slab hydration and intermediate-depth seismicity
inferred← citeshttps://doi.org/10.11606/t.14.2019.tde-29052018-081758openalex-snapshot
Serpentinites néoprotérozoïques : une fenêtre sur la lithosphère océanique associée à la dislocation de Rodinia
inferred← citeshttps://doi.org/10.1186/s40623-020-01352-6openalex-snapshot
Aqueous alteration without initial water: possibility of organic-induced hydration of anhydrous silicates in meteorite parent bodies
inferred← citeshttps://doi.org/10.1515/9783111437040-001openalex-snapshot
23Chapter 1 Evaluating natural hydrogen systems through the lens of petroleum exploration
inferred← citeshttps://doi.org/10.2138/am-2014-4825openalex-snapshot
The replacement of chalcopyrite by bornite under hydrothermal conditions
inferred← citeshttps://doi.org/10.2138/am-2015-5112openalex-snapshot
Experimental constraints on fluid-rock reactions during incipient serpentinization of harzburgite
inferred← citeshttps://doi.org/10.2138/am-2016-5772openalex-snapshot
Dissolution-reprecipitation and self-assembly of serpentine nanoparticles preceding chrysotile formation: Insights into the structure of proto-serpentine
inferred← citeshttps://doi.org/10.2138/am.2014.4606openalex-snapshot
Surface-specific measurements of olivine dissolution by phase-shift interferometry
inferred← citeshttps://doi.org/10.2138/gselements.19.3.165openalex-snapshot
Olivine—The Alteration Rock Star
inferred← citeshttps://doi.org/10.2138/rmg.2015.80.02openalex-snapshot
Pore-Scale Controls on Reaction-Driven Fracturing
inferred← citeshttps://doi.org/10.2475/001c.140951openalex-snapshot
A Micromechanical Model for Mineral Replacement Reactions and Associated Deformation: From Pore Clogging to Solid Volume Increase
inferred← citeshttps://doi.org/10.31223/x51k90openalex-snapshot
High-magnitude stresses induced by mineral-hydration reactions
inferred← citeshttps://doi.org/10.3389/feart.2017.00037openalex-snapshot
An Experimental Study of the Carbonation of Serpentinite and Partially Serpentinised Peridotites
inferred← citeshttps://doi.org/10.3389/feart.2019.00017openalex-snapshot
Hydrothermal Production of H2 and Magnetite From Steel Slags: A Geo-Inspired Approach Based on Olivine Serpentinization
inferred← citeshttps://doi.org/10.3390/app12083990openalex-snapshot
Influence of Petrogenesis on the Engineering Properties of Ultramafic Aggregates and on Their Suitability in Concrete
inferred← citeshttps://doi.org/10.3390/geosciences15030112openalex-snapshot
Quantifying Natural Hydrogen Generation Rates and Volumetric Potential in Onshore Serpentinization
inferred← citeshttps://doi.org/10.3390/min12010058openalex-snapshot
Petrographic Record and Conditions of Expansive Hydration of Anhydrite in the Recent Weathering Zone at the Abandoned Dingwall Gypsum Quarry, Nova Scotia, Canada
inferred← citeshttps://doi.org/10.3390/min6040104openalex-snapshot
Nano-Tomography of Porous Geological Materials Using Focused Ion Beam-Scanning Electron Microscopy
inferred← citeshttps://doi.org/10.3390/min7100190openalex-snapshot
The Force of Crystallization and Fracture Propagation during In-Situ Carbonation of Peridotite
inferred← citeshttps://doi.org/10.3390/min8060241openalex-snapshot
Deformation Processes, Textural Evolution and Weakening in Retrograde Serpentinites
inferred← citeshttps://doi.org/10.3390/min8090412openalex-snapshot
Intracrystalline Reaction-Induced Cracking in Olivine Evidenced by Hydration and Carbonation Experiments
inferred← citeshttps://doi.org/10.46427/gold2020.1828openalex-snapshot
Reaction-Induced Fracturing during Silicate Weathering and Carbonation
inferred← citeshttps://doi.org/10.5194/ejm-36-555-2024openalex-snapshot
H 2 mobility and redox control in open vs. closed hydrothermal oceanic systems – evidence from serpentinization experiments
inferred← citeshttps://doi.org/10.5194/se-13-1191-2022openalex-snapshot
Progressive veining during peridotite carbonation: insights from listvenites in Hole BT1B, Samail ophiolite (Oman)
inferred← citeshttps://doi.org/10.5194/se-17-537-2026openalex-snapshot
Impact of differential stress on fracture due to volume increasing hydration
inferred← citeshttps://doi.org/10.5194/se-2021-152openalex-snapshot
Progressive veining during peridotite carbonation: insights from listvenites in Hole BT1B, Samail ophiolite (Oman)
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