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%
• Titanomagnetite 100%
• Rock Magnetics 100%
• Single Domain 100%
• Magnetic Carrier 100%
• Susceptibility Profile 100%
• Century Scale 100%
• Debris 50%
• Magnetic Susceptibility 50%
• Magnetic Minerals 50%
• Rutile 50%
• Biogenic Sediment 50%
• Paleoenvironmental Conditions 50%
• Magnetic Mineralogy 50%
• Sediment Provenance 50%
• Western Antarctic Peninsula 50%
• Mineral Assemblage 50%
• Multi-domain 50%
• Sediment Transport Processes 50%
• Terrigenous Material 50%
• Glacial Sedimentation 50%
• Low Susceptibility 50%
• High Susceptibility 50%
• Superparamagnetic Particles 50%
• Millennial-scale Variability 50%
• Mid-Miocene Climatic Optimum 50%
• Multidomain Magnetite 50%
• Depth Records 50%
• Neoglacial Period 50%

Earth and Planetary Sciences

• Marine Sediment 100%
• Peninsula 100%
• Magnetite 100%
• Titanomagnetite 66%
• Multidomain 66%
• Earth Surface Sediment Transport 33%
• Magnetic Permeability 33%
• Magnetic Mineral 33%
• Mineralogy 33%
• Biogenic Deposit 33%
• Transport Process 33%
• Dilution 33%
• Neoglacial 33%
• Hypsithermal 33%
• Glacial Sedimentation 33%
• Magnetism 33%