Biochemical vs. detrital mechanism of remanence acquisition in marine carbonates: A lesson from the K-T boundary interval

Earth and Planetary Science Letters

Volumn 286, Issue 1-2, 2009, Pages 269-277

  Abrajevitch, Alexandra ^a   Kodama, Kazuto ^a  

^a KOCHI UNIVERSITY   (Japan)

Author keywords

biogenic magnetite; marine carbonates; oxyhydroxides; remanence; rock magnetism

Indexed keywords

AUTHIGENIC; BIOGENIC MAGNETITE; BIOGENIC ORIGINS; BIOLOGICAL ACTIVITIES; BIOLOGICAL PRODUCTIVITY; BIOTURBATION; BOUNDARY INTERVALS; CRETACEOUS-TERTIARY BOUNDARY; DOMINANT PROCESS; FERROMAGNETIC FRACTIONS; IRON OXYHYDROXIDES; IRON-BEARING PHASE; KERGUELEN PLATEAU; LAMINATED SEDIMENTS; LOCAL SOURCE; MAGNETIC STUDIES; MARINE CARBONATES; MARINE ENVIRONMENT; MULTI DOMAINS; NATURAL REMANENT MAGNETIZATION; NON-SILICATE; ORDER OF MAGNITUDE; OXYHYDROXIDES; PARAMAGNETIC PHASIS; REMANENT MAGNETIZATION; ROCK MAGNETISM; SINGLE DOMAINS;

CARBONATES; CLAY MINERALS; GEOMAGNETISM; LAMINATING; LITHOLOGY; MAGNETIC DOMAINS; MAGNETIC PROPERTIES; MAGNETITE; MAGNETIZATION; MAGNETS; MERGERS AND ACQUISITIONS; OXIDE MINERALS; ROCKS; SILICATES;

REMANENCE;

BIOCHEMISTRY; BIOTURBATION; CARBONATE; CRETACEOUS-TERTIARY BOUNDARY; DATA ACQUISITION; DETRITAL DEPOSIT; MAGNETITE; NATURAL REMANENT MAGNETIZATION; PALEOMAGNETISM; REMAGNETIZATION;

INDIAN OCEAN; KERGUELEN PLATEAU;

EID: 69549116235     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2009.06.035     Document Type: Article

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