Downcore variations of the S-ratio for CON01-603-2, CON01-604-2, CON01-605-3, VER98-1-1, VER98-1-14

Description: In interglacial sediments, the magnetic assemblages depict changes in the sedimentation rate, which are traced using the ratio of magnetite over hematite (S-ratio). At the beginning of interglacials, the sedimentation rate is constant with an assemblage magnetite+greigite (high S-ratio), and at the end of some interglacials, the sedimentation rate decreases with a predominance of hematite (low S-ratio).

Global identifier:

Doi(
    "10.1594/GFZ.SDDB.1035",
)

Origins: /Wissenschaft/GFZ

Tags: Sediment ? Berechnung ? Sedimentation ? R/V Vereshchagin ? Vereshchagin 98 Expedition ? Vereshchagin Long Cores Expedition 2001 ? s-ratio ?

License: unbekannt

Language: Englisch/English

Organisations

• Deutsches GeoForschungsZentrum GFZ (Herausgeber*in)

Issued: 2006-01-01

Time ranges: 2006-01-01 - 2006-01-01

Status

Aktiv

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• Accessibility: 0.67

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• Interoperability: 0.25

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• Reusability: 0.33

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