Experimental logs and analysis of olivine polymorphs and MORB (Mid-Ocean Ridge Basalt) composition garnetite samples recovered from high-pressure faulting experiments
Multi-anvil experiments were performed both in static and deformation geometries on olivine polymorphs and MORB (Mid-Ocean Ridge Basalt) -composition garnetite. Faults were induced by uniaxial compression in both garnetite and wadsleyite but only the garnetite showed evidence of thermal run away to melting. These results suggest that strain localisation by thermal feedback might be an important mechanism for triggering deep earthquakes in the crustal portion of subducted slabs in the deeper transition zone (~500-660 km depth).
nonGeographicDataset
https://webapps.bgs.ac.uk/services/ngdc/accessions/index.html#item186488
name: Data
function: download
https://doi.org/10.5285/7b24d391-ce38-42e2-a9d7-f2704d4ccf1f
name: Digital Object Identifier (DOI)
function: information
http://data.bgs.ac.uk/id/dataHolding/13608306
eng
geoscientificInformation
publication
2008-06-01
Deep seismic surveys
Basalt
MORB
Garnetite
NGDC Deposited Data
revision
2022
NERC_DDC
2022-11-01
2024-10-12
creation
2024-09-26
notApplicable
Samples were pre-synthesised at 15 GPa and 1473 K from synthetic glass of MORB composition, or from San-Carlos olivine, in platinum foil capsules. Recovered synthetic samples were prepared for deformation experiments using the deformation-T-cup press at UCL (see Hunt et al Rev. Sci. Instr. 85, 085103, 2014. doi: 10.1063/1.4891338). Ductile deformation was performed at 15 GPa and 1473 K in axial shortening mode. Further brittle faults were introduced into the sample during decompression. Recovered deformed sample was sectioned perpendicular to the faults and polished for SEM and chemical analyses at UCL. TEM foils were prepared and TEM analysis was performed at Imperial College.
publication
2011
false
See the referenced specification
publication
2010-12-08
false
See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF
pptx
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Professor of Earth Materials
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originator
University College London
originator
University College London
originator
University of Oxford
originator
British Geological Survey
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British Geological Survey
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British Geological Survey
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2025-05-25