<?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>2026-10-13T02:01:06Z</responseDate><request identifier="10.35097/hbwBDGIgWbcvTFYc" metadataPrefix="oai_dc" verb="GetRecord">https://www.radar-service.eu/oai/OAIHandler</request><GetRecord><record><header><identifier>10.35097/hbwBDGIgWbcvTFYc</identifier><datestamp>2026-10-09T11:03:55Z</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/hbwBDGIgWbcvTFYc</dc:identifier>
   <dc:creator>Fuchs, Helena</dc:creator>
   <dc:creator>Kontny, Agnes</dc:creator>
   <dc:creator>Reznik, Boris</dc:creator>
   <dc:creator>Schilling, Frank R.</dc:creator>
   <dc:title>Supplementary Data - Stress-induced Changes in Magnetite: Insights from a Numerical Analysis of the Verwey Transition</dc:title>
   <dc:publisher>Karlsruhe Institute of Technology</dc:publisher>
   <dc:date>2024</dc:date>
   <dc:subject>Geography</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-nc-sa/4.0/legalcode</dc:rights>
   <dc:description>The dataset contains measurements of magnetic susceptibility in dependence of temperature of shocked magnetite and of a natural magnetite single crystal before and after manual crushing. A python code for evaluation of low-temperature susceptibility curves is included. The data are supplementary to: Fuchs, H., Kontny, A. and Schilling, F.R., 2024. Stress-induced Changes in Magnetite: Insights from a Numerical Analysis of the Verwey Transition, Geophysical Journal International</dc:description>
   <dc:description>The data set contains k-T curves of &#xD;
- Initial magnetite ore from Sydvaranger mine (Norway)&#xD;
- the same ore after shock at 3, 5, 10, 20 and 30 GPa under laboratory conditions and after subsequent heating to 973 K&#xD;
-Natural magnetite single crystal (initial and after manual crushing)&#xD;
The data set contains a python code for evaluation of normalized low-temperature k-T curves.&#xD;
Experimental conditions are described in [1]. The approach for k-T curve evaluation is described in [2]&#xD;
&#xD;
[1]: Kontny, A., Reznik, B., Boubnov, A., Göttlicher, J. and Steininger, R., 2018. Postshock Thermally Induced Transformations in Experimentally Shocked Magnetite, Geochemistry, Geophysics, Geosystems, Vol. 19, 3, pp. 921–931, doi:10.1002/2017GC007331.&#xD;
[2] Fuchs, H., Kontny, A. and Schilling, F.R., 2024. Stress-induced Changes in Magnetite: Insights from a Numerical Analysis of the Verwey Transition, Geophysical Journal International</dc:description>
   <dc:subject>Magnetic susceptibility</dc:subject>
   <dc:subject>Magnetite</dc:subject>
   <dc:format>application/x-tar</dc:format>
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