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        <identifier>doi:10.1594/pangaea.510751</identifier>
        <datestamp>2026-05-03T03:36:25Z</datestamp>
        <setSpec>PANGAEA</setSpec>
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          <dc:title>Petrophysical investigations on sediment core CRP-2A from the Ross Sea, Antarctica</dc:title>
          <dc:creator>Brink, Jason</dc:creator>
          <dc:creator>Jarrard, Richard D</dc:creator>
          <dc:publisher>PANGAEA</dc:publisher>
          <dc:date>2000</dc:date>
          <dc:date>Issued: 2000</dc:date>
          <dc:relation>handle:10013/epic.28278.d001</dc:relation>
          <dc:subject>Core wireline system</dc:subject>
          <dc:subject>CRP-2__Campaign</dc:subject>
          <dc:subject>Sampling/drilling from ice</dc:subject>
          <dc:subject>Cape Roberts Project (CRP)</dc:subject>
          <dc:description>A suite of petropysical measurements - velocity versus pressure, bulk density, porosity, matrix density, and magnetic susceptibility -was undertaken on 63 core plugs from CRP-2A. These data are used to calibrate neutron, resistivity, and magnetic susceptibility well logs. Agreement between core-plug magnetic susceptibility measurements and both well-log and whole-core data is excellent. Comparison of core-plug bulk densities with continious well-log density records shows very good agreement. Core-plug measurements of matrix density permit conversion of the well-log and whole-core density records to porosity. Sands and muds exhibit similar downhole compaction patterns, and both patterns are consistent with 250 ± 150 m of exhumation. Pervasive cementation, particularly in the lower half of the core, has affected many CRP-2A petrophysical parameters:(1) fractional porosities are reduced by about 0.05 - 0.10 in the lower part of the hole;(2) velocity and porosity rebound are much smaller than is usually observed for unconsolidated sediments with burial depths similar to CRP-2A;(3) velocities are unusually insensitive to pressure, suggesting that any exhumation-induced microcracks have been scaled subsequently;(4) the velocity/porosity relationship lacks the characteristic signature of exhumation-induced microcracks;(5) the velocity/porosity relationship changes with depth, indicating downhole increase in consolidation;(6) Vp/Vs ratios of the highest-porosity sediments are unusually low, implying enhancement of framework stiffness.</dc:description>
          <dc:description>Supplement to: Brink, Jason; Jarrard, Richard D (2000): Petrophysics of core plugs from CRP-2A drillhole, Victoria Land Basin, Antarctica. Terra Antartica, 7(3), 231-240</dc:description>
          <dc:language>en</dc:language>
          <dc:type>Collection</dc:type>
          <dc:type>Supplementary Publication Series of Datasets</dc:type>
          <dc:format>application/zip</dc:format>
          <dc:rights>Creative Commons Attribution 3.0 Unported</dc:rights>
          <dc:rights>https://creativecommons.org/licenses/by/3.0/legalcode</dc:rights>
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