Plastically deforming clay-rich sediment to help measure the average remanence anisotropy of its individual magnetic particles, and correct for paleomagnetic inclination shallowing

Physics and Chemistry of the Earth

Volumn 27, Issue 25-31, 2002, Pages 1273-1279

  Hodych, J P ^a   Bijaksana, S ^b  

^a MEMORIAL UNIVERSITY OF NEWFOUNDLAND   (Canada)

^b BANDUNG INSTITUTE OF TECHNOLOGY   (Indonesia)

Author keywords

Magnetic anisotropy; Magnetic inclination; Paleomagnetism; Sediments

Indexed keywords

MAGNETIC ANISOTROPY; MAGNETIC FIELDS; MAGNETITE; PLASTIC DEFORMATION;

REMANENCE INCLINATION;

REMANENCE;

CLAY; MAGNETIC ANISOTROPY; MAGNETIC INCLINATION; PALEOMAGNETISM; PLASTIC DEFORMATION;

EID: 0036433955     PISSN: 14747065     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1474-7065(02)00112-2     Document Type: Article

References (10)

1. Comparing remanence anisotropy and susceptibility anisotropy as predictors of paleomagnetic inclination shallowing in turbidites from the Scotian Rise
2. Hysteresis properties of titanomagnetites: Grain size and compositional dependence
3. Can remanence anisotropy detect paleomagnetic inclination shallowing due to compaction? A case study using Cretaceous deep-sea limestones
4. Using magnetic anisotropy to correct for paleomagnetic inclination shallowing in some magnetite-bearing deep-sea turbidites and limestones
5. Pre-history of the Earth's magnetic field
6. Detrital remanence, inclination errors and anhysteretic remanence anisotropy: Quantitative model and experimental results
7. A successful rock magnetic technique of correcting paleomagnetic inclination shallowing: Case study of the Naciemento Formation. New Mexico
8. A compaction correction for the paleomagnetism of the Cretaceous Pigeon Point Formation of California
9. Compaction-corrected inclinations from southern California Cretaceous marine sedimentary rocks indicate no paleolatitudinal offset for the Peninsular Ranges terrane