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<md:author id="dataset.author41786">
<md:lastName>Tanaka</md:lastName>
<md:firstName>Chihiro</md:firstName>
</md:author>
<md:author id="dataset.author594">
<md:lastName>Ogawa</md:lastName>
<md:firstName>Yujiro</md:firstName>
</md:author>
<md:year>2006</md:year>
<md:title>(Table T1) Density, porosity, void ratio and silica crystallinity index of ODP Site 185-1149 sediments</md:title>
<md:type id="dataset.reftype10" includeInCitation="true">dataset</md:type>
<md:URI>https://doi.org/10.1594/PANGAEA.784110</md:URI>
<md:supplementTo id="ref36543">
<md:author id="ref36543.author41786">
<md:lastName>Tanaka</md:lastName>
<md:firstName>Chihiro</md:firstName>
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<md:author id="ref36543.author594">
<md:lastName>Ogawa</md:lastName>
<md:firstName>Yujiro</md:firstName>
</md:author>
<md:year>2006</md:year>
<md:title>Data report: Silica mineral crystallization with textural change of Cretaceous siliceous/calcareous pelagic sedimentary rocks recovered from the northwest Pacific, ODP Leg 185</md:title>
<md:type id="ref36543.reftype15">book chapter</md:type>
<md:source>In: Ludden, JN; Plank, T; Escutia, C (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program)</md:source>
<md:volume>185</md:volume>
<md:URI>https://doi.org/10.2973/odp.proc.sr.185.004.2006</md:URI>
<md:pages>1-11</md:pages>
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<md:abstract>Siliceous pelagic sediments have been known to be crystallographically altered during burial diagenesis (e.g., Hesse, 1990; Behl and Smith, 1992, doi:10.2973/odp.proc.sr.129.112.1992). In order to know the systematic downhole change of silicification, sediments from Pacific Ocean crust obtained during Ocean Drilling Program Leg 185 Site 1149 (Plank, Ludden, Escutia, et al., 2000, doi:10.2973/odp.proc.ir.185.2000) were analyzed. For collected samples of Early Cretaceous age below the pelagic sediments, which are not as highly silicified, silica mineral crystallization in the siliceous sedimentary rocks is determined by X-ray diffraction (XRD), and the related textural change is shown by using scanning electron microscope (SEM).</md:abstract>
<md:extent>
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<md:eastBoundLongitude>143.4004</md:eastBoundLongitude>
<md:southBoundLatitude>31.3132</md:southBoundLatitude>
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<md:name>Ocean Drilling Program, Texas A&amp;M University</md:name>
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<md:comment>23 cores; 191.2 m cored; 0 m drilled; 91.2 % recovery</md:comment>
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<md:comment>31 core; 284.6 m cored; 151.1 m drilled; 11.6 % recovery</md:comment>
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<md:attribute attid="19162" name="Penetration">426.7 m</md:attribute>
<md:attribute attid="19163" name="Recovery">6.39 m</md:attribute>
<md:comment>8 cores; 76.9 m cored; 0 m drilled; 8.3 % recovery</md:comment>
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<md:comment>18 cores; 168.2 m cored; 0 m drilled; 17.1 % recovery</md:comment>
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<md:label>CC-BY-3.0</md:label>
<md:name>Creative Commons Attribution 3.0 Unported</md:name>
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<md:comment>mbsf</md:comment>
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<md:comment>d(101) spacing of cristobalite, 2 theta</md:comment>
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<md:caption>Density [g/cm**3]</md:caption>
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<md:lastName>Tanaka</md:lastName>
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<md:comment>silica crystallinity index, after Murata and Norman (1976, doi:10.2475/ajs.276.9.1120)</md:comment>
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