<?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_785120</Entry_ID>
<Entry_Title>(Table 2) CT scan measurements of ODP Site 131-808</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Soh, Wonn; Byrne, Timothy; Taira, Asahiko; Kono, Atsushi</Dataset_Creator>
<Dataset_Title>(Table 2) CT scan measurements of ODP Site 131-808</Dataset_Title>
<Dataset_Release_Date>1993</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Other_Citation_Details>Supplement to: Soh, Wonn; Byrne, Timothy; Taira, Asahiko; Kono, Atsushi (1993): Computed tomography (CT) scan image analysis of Site 808 cores: structural and physical property implications. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 135-140, https://doi.org/10.2973/odp.proc.sr.131.113.1993</Other_Citation_Details>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.785120</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Wonn</First_Name>
<Last_Name>Soh</Last_Name>
</Personnel>
<Personnel>
<Role>Investigator</Role>
<First_Name>Asahiko</First_Name>
<Last_Name>Taira</Last_Name>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>Sample code/label</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DEPTH, sediment/rock</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Attenuation value</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Attenuation value, standard deviation</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sample comment</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Density, wet bulk</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Porosity</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>131-808</Keyword>
<Keyword>Composite Core</Keyword>
<Keyword>Leg131</Keyword>
<Sensor_Name>
<Long_Name>DSDP/ODP/IODP sample designation</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>X-ray computed tomography (CT)</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>Joides Resolution</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>1990-04-04</Start_Date>
<Stop_Date>1990-05-31</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>32.35215</Southernmost_Latitude>
<Northernmost_Latitude>32.35215</Northernmost_Latitude>
<Westernmost_Longitude>134.944366666666</Westernmost_Longitude>
<Easternmost_Longitude>134.944366666666</Easternmost_Longitude>
<Minimum_Depth>43.2 m (DEPTH, sediment/rock)</Minimum_Depth>
<Maximum_Depth>1262.6 m (DEPTH, sediment/rock)</Maximum_Depth>
</Spatial_Coverage>
<Project>
<Short_Name>ODP</Short_Name>
<Long_Name>Ocean Drilling Program</Long_Name>
</Project>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-3.0: Creative Commons Attribution 3.0 Unported</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>
</Contact_Address>
</Personnel>
</Data_Center>
<Distribution>
<Distribution_Media>online</Distribution_Media>
<Distribution_Size>116 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Taira, Asahiko; Hill, Ian Ashley; Firth, John V; Berner, Ulrich; Brückmann, Warner; Byrne, Timothy; Chabernau, T; Fisher, Andrew T; Foucher, Jean Paul; Gamo, Toshitaka; Gieskes, Joris M; Hyndman, Roy D; Karig, Daniel E; Kastner, Miriam; Kato, Yukihiro; Lallemant, Siegfried J; Lu, Ran; Maltman, Alex J; Moore, Gerald F; Moran, K; Olafsson, Gunnar; Owens, W Brechner; Pickering, Kevin T; Siena, Franca; Taylor, Elliott; Underwood, Michael B; Wilkinson, Clive; Yamano, Makoto; Zhang, J (1992): Sediment deformation and hydrogeology of the Nankai Trough accretionary prism: Synthesis of shipboard results of ODP Leg. Earth and Planetary Science Letters, 109(3-4), 431-450, https://doi.org/10.1016/0012-821X(92)90104-4</Reference>
<Summary>X-ray computed tomography (CT) is a promising tool that yields data useful for understanding the fine-scale density structure of partly lithified and tectonically deformed sediments. We conducted 21 CT scans of ODP Leg 131 sediments, including whole-round cores and thin-section chips, obtained from the toe of the Nankai accretionary prism. The samples range from highly deformed pieces from the frontal thrust and décollement to homogeneous and essentially undeformed sediments above the frontal thrust and beneath the décollement. In the CT images, kink-like deformation bands and faults are recognized as obvious bright seams, bands, or stripes with relatively high linear attenuation coefficients. The differences in linear attenuation coefficients relative to the matrix range from 0.021 cm**2/g (kink-like deformation band) to 0.038 cm**2/g (fault). These data suggest a 0.10 g/cm**3 to 0.18 g/cm**3 increase in bulk density within the deformation structures, and they appear to be 13% and 33% more compacted than the nondeformed matrix, respectively. In contrast to the samples from the frontal thrust zone, CT images of the décollement sample exhibit relatively homogeneous textures. The attenuation coefficient of the sample of the décollement indicates bulk density and porosity values of 2.45 g/cm**3 and 18%, respectively. The sample, hence, is approximately 50% more compacted than the sediment outside the décollement zone. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.785120"!</Summary>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/Porosity</URL>
<Description>Porosity</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/0012-821X(92)90104-4</URL>
<Description>Sediment deformation and hydrogeology of the Nankai Trough accretionary prism: Synthesis of shipboard results of ODP Leg</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.2973/odp.proc.sr.131.113.1993</URL>
<Description>Computed tomography (CT) scan image analysis of Site 808 cores: structural and physical property implications</Description>
</Related_URL>
<Related_URL>
<URL>https://hdl.handle.net/10013/epic.27914.d001</URL>
<Description>DSDP/ODP/IODP sample designation</Description>
</Related_URL>
<Related_URL>
<URL>https://www-odp.tamu.edu:443/</URL>
<Description>ODP</Description>
</Related_URL>
<Related_URL>
<URL>https://www-odp.tamu.edu:443/resolutn.html</URL>
<Description>Joides Resolution</Description>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date/>
<Last_DIF_Revision_Date>2026-08-12</Last_DIF_Revision_Date>
</DIF>
