Modelled depth and thermal history for sediments offshore Sumatra (NERC grant NE/P012140/1)
The thermal state of marine sediments controls a range of potential dehydration reactions as sediments are subducted. In thick sediment sections it is possible that reactions that would normally occur within a subduction zone start offshore of the deformation front. This scenario may be occurring at the Sumatra subduction zone (e.g. Geersen et al., 2013; Huepers et al., 2017). We have investigated this possibility by modelling the thermal and depth history of sediments offshore Sumatra. We have used a range of different assumptions about how the sediments decompact with depth, as well as testing the dependence on the seismic velocities used for depth conversion of the horizons.
nonGeographicDataset
http://www.bgs.ac.uk/services/ngdc/accessions/index.html#item107290
function: information
http://data.bgs.ac.uk/id/dataHolding/13607280
eng
geoscientificInformation
publication
2008-06-01
Subduction
Sedimentary history
Seismic velocity
NGDC Deposited Data
Marine sediments
Subduction zones
revision
2022
NERC_DDC
2017-02-01
2017-07-01
revision
2018-02-15
notApplicable
The data are generated using SlugSed modelling software (Hutnak and Fisher, 2007) using a range of different scenarios to account for variations due to parameters that are poorly constrained.
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
Text files
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Professor of Geophysics
University of Southampton
National Oceanography Centre, European Way
Southampton
SO14 3ZH
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British Geological Survey
Environmental Science Centre,Keyworth
NOTTINGHAM
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United Kingdom
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2025-05-04