Updated Geomagnetic Field Variations during the Past 1,500 Years in Georgia, U.S.S.R.
S. P. Burlatskaya, Z. A. Chelidze
Abstract
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S. P. Burlatskaya, Z. A. Chelidze
Abstract
Open-access reader
155 samples from 170 collected at 36 archaeological sites dating between the 15th and 1st century B. C. defines the variation in declination (±20°), inclination (±10°) and ancient intensity (±15-20μT) in Georgia. These new observations are consistent with earlier observations and, when combined with them, these errors are reduced to ±5°, ±4°, and ±5-6μT. The virtual dipole path shows an anticlockwise rotation during this period.
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155 samples from 170 collected at 36 archaeological sites dating between the 15th and 1st century B. C. defines the variation in declination (±20°), inclination (±10°) and ancient intensity (±15-20μT) in Georgia. These new observations are consistent with earlier observations and, when combined with them, these errors are reduced to ±5°, ±4°, and ±5-6μT. The virtual dipole path shows an anticlockwise rotation during this period.
Key concepts: Declination, Clockwise, Earth's magnetic field, Magnetic declination, Paleomagnetism, Geology, Geodesy, Geomagnetic pole