<?xml version="1.0" encoding="UTF-8" ?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-10-12T15:15:48Z</responseDate><request identifier="10.35097/1289" metadataPrefix="oai_dc" verb="GetRecord">https://www.radar-service.eu/oai/OAIHandler</request><GetRecord><record><header><identifier>10.35097/1289</identifier><datestamp>2026-10-09T11:06:11Z</datestamp><setSpec>radar4kit</setSpec></header><metadata><oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/"
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   <dc:identifier>https://dx.doi.org/10.35097/1289</dc:identifier>
   <dc:creator>Braszus, Benedikt</dc:creator>
   <dc:creator>Rietbrock, Andreas</dc:creator>
   <dc:title>VoiLA-P19: A 3-D P-wave velocity model of the upper mantle beneath the Caribbean derived from teleseismic travel time tomography</dc:title>
   <dc:publisher>Karlsruhe Institute of Technology</dc:publisher>
   <dc:date>2023</dc:date>
   <dc:subject>Physics</dc:subject>
   <dc:type>dataset</dc:type>
   <dc:subject>Dataset</dc:subject>
   <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
   <dc:rights>https://creativecommons.org/licenses/by/4.0/legalcode</dc:rights>
   <dc:contributor>Goes, Saskia</dc:contributor>
   <dc:contributor>Allen, Rob</dc:contributor>
   <dc:contributor>Collier, Jenny</dc:contributor>
   <dc:description>##   README   &#xD;
# ___________________&#xD;
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### VoiLA-P19: A 3-D P-wave velocity model of the upper mantle beneath the Caribbean derived from teleseismic travel time tomography &#xD;
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The files layer_XX.xyz (with XX indicating the number of the layer from 01-08) contain P-wave velocity anomalies (3rd column) in % with reference to the AK135 model at given longitudes (1st column) ranging from -73.5° to -57.0° and latitudes (2nd column) ranging from 6.5° to 23.0° with increments of 0.05° in both longitude and latitude. &#xD;
The files layer_XX.grd contain the same model as .grd-files. &#xD;
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The 8 layers of the model correspond to the following depth ranges:&#xD;
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  0- 40 km : layer01&#xD;
 40-100 km : layer02&#xD;
100-160 km : layer03&#xD;
160-240 km : layer04&#xD;
230-320 km : layer05&#xD;
320-410 km : layer06&#xD;
410-530 km : layer07&#xD;
530-660 km : layer08&#xD;
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A GMT script 'plot_layers.gmt' is provided to plot horizontal slices of the velocity anomalies. &#xD;
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More information on the final model and a suggested set of interpretations can be found in:&#xD;
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        Braszus, B., et al. (2021), Subduction history of the Caribbean from upper-mantle seismic imaging and plate reconstruction, Manuscript in revision for Nature Communications.&#xD;
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Further details of the method and tests for an earlier version of the model are in:&#xD;
&#xD;
        Braszus, B. (2019), 3D teleseismic travel time tomography along the Lesser Antilles subduction zone, 83 pp, Karlsruhe Institute of Technology, Karlsruhe, Germany, doi:10.5445/IR/1000124003.</dc:description>
   <dc:subject>teleseismic P-wave travel time tomography</dc:subject>
   <dc:subject>Caribbean</dc:subject>
   <dc:contributor>Goes, Saskia</dc:contributor>
   <dc:contributor>Allen, Rob</dc:contributor>
   <dc:contributor>Collier, Jenny</dc:contributor>
   <dc:identifier>10.5445/IR/1000130417</dc:identifier>
   <dc:identifier>KITopen-DOI</dc:identifier>
   <dc:format>application/x-tar</dc:format>
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