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Single crystal elasticity of lawsonite

American Mineralogist (2000) 85 (11-12): 1834–1837.
This article has been cited by the following articles in journals that are participating in CrossRef Cited-by Linking.
Twin Induced Reduction of Seismic Anisotropy in Lawsonite Blueschist
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Experimentally deformed lawsonite at high pressure and high temperature: Implication for low velocity layers in subduction zones
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Poisson's Ratio and Auxetic Properties of Natural Rocks
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Petrogenesis and deformation history of the lawsonite‐bearing blueschist facies metabasalts of the Diamante‐Terranova oceanic unit (southern Italy)
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Seismic properties and anisotropy of the continental crust: Predictions based on mineral texture and rock microstructure
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Reviews of Geophysics (2017) 55 (2): 367.
Seismic properties of lawsonite eclogites from the southern Motagua fault zone, Guatemala
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Tectonophysics (2016) 677-678: 88.
Seismic properties of subducting oceanic crust: Constraints from natural lawsonite-bearing blueschist and eclogite in Sivrihisar Massif, Turkey
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Physics of the Earth and Planetary Interiors (2016) 250: 12.
High-pressure behavior of natural single-crystal epidote and clinozoisite up to 40 GPa
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Physics and Chemistry of Minerals (2016) 43 (9): 649.
Effect of hydration on the elasticity of mantle minerals and its geophysical implications
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Science China Earth Sciences (2016) 59 (5): 873.
Thermal equation of state of lawsonite up to 10 GPa and 973 K
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Fluid/melt in continental deep subduction zones: Compositions and related geochemical fractionations
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Science China Earth Sciences (2015) 58 (9): 1457.
Microstructures and petro-fabrics of lawsonite blueschist in the North Qilian suture zone, NW China: Implications for seismic anisotropy of subducting oceanic crust
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Tectonophysics (2014) 628: 140.
Lawsonite geochemistry and stability – implication for trace element and water cycles in subduction zones
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Elasticity of lawsonite and seismological signature of metamorphism and water cycling in the subducting oceanic crust
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Lawsonite blueschists and lawsonite eclogites as proxies for palaeo‐subduction zone processes: a review
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Journal of Metamorphic Geology (2014) 32 (5): 437.
Petro-fabrics and seismic properties of blueschist and eclogite in the North Qilian suture zone, NW China: Implications for the low-velocity upper layer in subducting slab, trench-parallel seismic anisotropy, and eclogite detectability in the subduction z
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Deformation fabrics of natural blueschists and implications for seismic anisotropy in subducting oceanic crust
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Physics of the Earth and Planetary Interiors (2013) 222: 8.
The elasticity of lawsonite at high pressure and the origin of low velocity layers in subduction zones
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Earth and Planetary Science Letters (2012) 349-350: 116.
The low velocity layer in subduction zone: Structure and elasticity of glaucophane at high pressures
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Physics of the Earth and Planetary Interiors (2012) 208-209: 50.
Experimental Measurements of Trace Element Partitioning Between Lawsonite, Zoisite and Fluid and their Implication for the Composition of Arc Magmas
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Journal of Petrology (2011) 52 (6): 1049.
P-wave velocity and anisotropy of lawsonite and epidote blueschists: Constraints on water transportation along subducting oceanic crust
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Physics of the Earth and Planetary Interiors (2010) 183 (1-2): 219.
Trench-parallel fast axes of seismic anisotropy due to fluid-filled cracks in subducting slabs
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Earth and Planetary Science Letters (2009) 283 (1-4): 75.
Sound velocities and elasticity of DHMS phase A to high pressure and implications for seismic velocities and anisotropy in subducted slabs
  • Carmen Sanchez-Valle
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  • Joseph R. Smyth
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Physics of the Earth and Planetary Interiors (2008) 170 (3-4): 229.
Single-crystal elasticity of diaspore, AlOOH, to 12GPa by Brillouin scattering
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Physics of the Earth and Planetary Interiors (2008) 170 (3-4): 221.
Single-crystal elastic properties of lawsonite and their variation with temperature
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Physics of the Earth and Planetary Interiors (2003) 136 (1-2): 107.
Metamorphic controls on seismic velocity of subducted oceanic crust at 100–250 km depth
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Earth and Planetary Science Letters (2002) 204 (1-2): 61.
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