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Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
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Hydraulic sealing due to pressure solution contact zone growth in siliciclastic rock fractures
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Characteristics of magma‐driven hydrothermal systems at oceanic spreading centers
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Some experimental and theoretical observations on the kinetics of hydration reactions with particular reference to serpentinization
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Rate of serpentinization in seafloor environments
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Reaction-driven cracking during retrograde metamorphism: Olivine hydration and carbonation
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Incipient hydration of mantle lithosphere at ridges: A reactive-percolation experiment
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Non-linear regimes of fluid flow in rock fractures
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Structure, permeability, and strength of a fault zone in the footwall of an oceanic core complex, the Central Dome of the Atlantis Massif, Mid-Atlantic Ridge, 30°N
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Deep permeability of the San Andreas Fault from San Andreas Fault Observatory at Depth (SAFOD) core samples
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Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14′N, MAR)
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Evolution of strength recovery and permeability during fluid–rock reaction in experimental fault zones
inferredcites →https://doi.org/10.1016/s0012-821x(03)00263-2openalex-snapshot
Serpentinization of the forearc mantle
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Laboratory study of fault healing and lithification in simulated fault gouge under hydrothermal conditions
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Permeability of fault-related rocks, and implications for hydraulic structure of fault zones
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Experimental Study of Carbon Sequestration Reactions Controlled by the Percolation of CO 2 -Rich Brine through Peridotites
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Permeability reduction in granite under hydrothermal conditions
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Discovery of ancient and active hydrothermal systems along the ultra‐slow spreading Southwest Indian Ridge 10°–16°E
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Permeability reduction of a natural fracture under net dissolution by hydrothermal fluids
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Dynamic control on serpentine crystallization in veins: Constraints on hydration processes in oceanic peridotites
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Serpentinization of oceanic peridotites: 2. Kinetics and processes of San Carlos olivine hydrothermal alteration
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Emplacement of mantle rocks in the seafloor at mid‐ocean ridges
inferredcites →https://doi.org/10.1029/97jb03402openalex-snapshot
Healing and sealing of a simulated fault gouge under hydrothermal conditions: Implications for fault healing
inferredcites →https://doi.org/10.1029/98jb02229openalex-snapshot
Precipitation sealing and diagenesis: 1. Experimental results
inferredcites →https://doi.org/10.1029/98jb02230openalex-snapshot
Precipitation sealing and diagenesis: 2. Theoretical analysis
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A new mechanism of slip weakening and strength recovery of friction associated with the mechanical consolidation of gouge
inferredcites →https://doi.org/10.1029/rg013i001p00057openalex-snapshot
Structure and constitution of the lower oceanic crust
inferredcites →https://doi.org/10.1029/wr016i006p01016openalex-snapshot
Validity of Cubic Law for fluid flow in a deformable rock fracture
inferredcites →https://doi.org/10.1029/wr020i009p01209openalex-snapshot
The Effect of Tortuosity on Fluid Flow Through a Single Fracture
inferredcites →https://doi.org/10.1038/35084000openalex-snapshot
An off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30° N
inferredcites →https://doi.org/10.1038/385329a0openalex-snapshot
Corrugated slip surfaces formed at ridge–transform intersections on the Mid-Atlantic Ridge
inferredcites →https://doi.org/10.1038/ncomms1636openalex-snapshot
Hydrothermal vent fields and chemosynthetic biota on the world's deepest seafloor spreading centre
inferredcites →https://doi.org/10.1046/j.0956-540x.2000.01280.xopenalex-snapshot
The abundance of ultramafic rocks in Atlantic Ocean crust
inferredcites →https://doi.org/10.1093/petrology/egp004openalex-snapshot
Onset and Progression of Serpentinization and Magnetite Formation in Olivine-rich Troctolite from IODP Hole U1309D
inferredcites →https://doi.org/10.1126/science.1085582openalex-snapshot
30,000 Years of Hydrothermal Activity at the Lost City Vent Field
inferredcites →https://doi.org/10.1126/science.265.5178.1558openalex-snapshot
Reduction of Permeability in Granite at Elevated Temperatures
inferredcites →https://doi.org/10.1130/0016-7606(1971)82[897:pagnos]2.0.co;2openalex-snapshot
Petrologic and Geophysical Nature of Serpentinites
inferredcites →https://doi.org/10.1130/0091-7613(1992)020<0705:sttvpi>2.3.co;2openalex-snapshot
Solution to the volume problem in serpentinization
inferredcites →https://doi.org/10.1130/g33390.1openalex-snapshot
The interface-scale mechanism of reaction-induced fracturing during serpentinization
inferredcites →https://doi.org/10.2136/sssaj1973.03615995003700040004xopenalex-snapshot
Dynamics of Fluids in Porous Media
inferredcites →https://doi.org/10.2138/am-2015-5112openalex-snapshot
Experimental constraints on fluid-rock reactions during incipient serpentinization of harzburgite
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