Rock-magnetic carriers of century-scale susceptibility cycles in glacial-marine sediments from the Palmer Deep, Antarctic Peninsula

Keyphrases

• Iron Oxide 100%
• Antarctic Peninsula 100%
• Marine Sediments 100%
• Rock Magnetics 100%
• Magnetic Carrier 100%
• Titanomagnetite 66%
• Single Domain 66%
• Multi-domain 66%
• Susceptibility Profile 66%
• Middle Eocene Climatic Optimum 33%
• Debris 33%
• Magnetic Susceptibility 33%
• Magnetic Minerals 33%
• Rutile 33%
• Biogenic Sediment 33%
• Paleoenvironmental Conditions 33%
• Magnetic Mineralogy 33%
• Sediment Provenance 33%
• Western Antarctic Peninsula 33%
• Mineral Assemblage 33%
• Sediment Transport Processes 33%
• Terrigenous Material 33%
• Glacial Sedimentation 33%
• Neoglacial 33%
• Low Susceptibility 33%
• High Susceptibility 33%
• Superparamagnetic Particles 33%
• Millennial-scale Variability 33%

Earth and Planetary Sciences

• Marine Sediment 100%
• Titanomagnetite 100%
• Multidomain 100%
• Peninsula 100%
• Earth Surface Sediment Transport 50%
• Magnetic Permeability 50%
• Magnetic Mineral 50%
• Mineralogy 50%
• Biogenic Deposit 50%
• Transport Process 50%
• Dilution 50%
• Neoglacial 50%
• Hypsithermal 50%
• Glacial Sedimentation 50%