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S-ratios of sediment core PS69/288-3

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PANGAEA2017-01-01 更新2026-04-09 收录
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https://doi.pangaea.de/10.1594/PANGAEA.874150
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资源简介:
IRM subsequently acquired in oppositely directed fields of 100 mT (IRM-100) and 300 mT (IRM-300) was measured in order to estimate the ratio of low- ([titano-]magnetite/maghemite) to high-coercive (hematite, goethite) magnetic minerals by calculation of S-100 = IRM-100/IRM700 and S-300 = IRM-300/IRM700 ratios (Liu et al., 2012)
提供机构:
Wiers, Steffen; Hillenbrand, Claus-Dieter; Ehrmann, Werner; Smith, James A; Kuhn, Gerhard; Nitsche, Frank-Oliver; Mogollón, José M; Kasten, Sabine; Klages, Johann Philipp; Frederichs, Thomas
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2017-01-01
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