作者: Martin J. Aitken , Adrian L. Allsop , Gillian D. Bussell , Mona B. Winter
DOI: 10.1016/0031-9201(89)90035-6
关键词: Pottery 、 Earth's magnetic field 、 Geology 、 Paleontology 、 Intensity (heat transfer) 、 Dipole 、 Moment (mathematics) 、 Variation (astronomy) 、 Latitude 、 Disturbance (geology) 、 Physics and Astronomy (miscellaneous) 、 Space and Planetary Science 、 Astronomy and Astrophysics 、 Geophysics
摘要: Abstract Thellier-type determinations of the ancient geomagnetic intensity are reported for a large number samples from Greece, comprising pottery and other archaeologically dated forms baked clay. Comparison is made with results parts world about same latitude: Near East, China western U.S.A. These data indicate that, in time-range studied, variation dipole moment unlikely to have been dominant influence; it suggested that westward drift non-dipole disturbance could responsible.