<?xml version="1.0" encoding="UTF-8"?><!--*** Generated from internal PANGAEA metadata schema by dif.xslt ***--><DIF xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.4.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/">
<Entry_ID>PANGAEA_900085</Entry_ID>
<Entry_Title>Clast size distribution data, photographs and code for numerical model</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Melosh, Benjamin</Dataset_Creator>
<Dataset_Title>Clast size distribution data, photographs and code for numerical model</Dataset_Title>
<Dataset_Release_Date>2019-04-04</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Other_Citation_Details>Supplement to: Melosh, Benjamin (2019): Fault initiation in serpentinite. Geochemistry, Geophysics, Geosystems, https://doi.org/10.1029/2018GC008092</Other_Citation_Details>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.900085</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Benjamin</First_Name>
<Last_Name>Melosh</Last_Name>
<Email>bmelosh@usgs.gov</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
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<Detailed_Variable>File name</Detailed_Variable>
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<Detailed_Variable>File format</Detailed_Variable>
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<Detailed_Variable>File size</Detailed_Variable>
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<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-4.0: Creative Commons Attribution 4.0 International</Use_Constraints>
<Data_Set_Language>English</Data_Set_Language>
<Data_Center>
<Data_Center_Name>
<Short_Name>PANGAEA</Short_Name>
<Long_Name>Data Publisher for Earth &amp; Environmental Science</Long_Name>
</Data_Center_Name>
<Data_Center_URL>https://www.pangaea.de/</Data_Center_URL>
<Personnel>
<Role>Data Center Contact</Role>
<First_Name>Michael</First_Name>
<Last_Name>Diepenbroek</Last_Name>
<Email>info@pangaea.de</Email>
<Contact_Address>
<Address>Leobener Str.</Address>
<City>Bremen</City>
<Province_or_State>Bremen</Province_or_State>
<Postal_Code>28359</Postal_Code>
<Country>Germany</Country>
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<Distribution_Media>online</Distribution_Media>
<Distribution_Size>12 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
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<Summary>Serpentinite is influential to plate tectonics and the strength of faults, however the influence deformation textures have on the evolution of fault strength is poorly understood. Using a range of unsheared to sheared serpentinite outcrops I investigate the progression of deformation during the initiation of faults in serpentinite. This is complimented with a detailed clast size distribution analysis and a numerical model to query the bulk rheology and distribution of stress during deformation. This study demonstrates primary serpentinization textures impact the strength and development of faults throughout their history. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.900085"!</Summary>
<Related_URL>
<URL>https://doi.org/10.1029/2018GC008092</URL>
<Description>Fault initiation in serpentinite</Description>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2019-04-04</DIF_Creation_Date>
<Last_DIF_Revision_Date>2024-07-19</Last_DIF_Revision_Date>
</DIF>
