Archeomagnetic and paleomagnetic dating

Among a total of 90 samples from hearths remains of six dwelling sites, the characteristic remanent magnetization components were isolated from 70 samples using the progressive alternating field demagnetizations and considered to record faithfully a thermoremanent magnetization at the timing of the last cooling of the hearths.

Two different approaches were made to determine the archeomagnetic ages: One is the conventional method using the relocated paleosecular variation (PSV) curve obtained from southwestern Japan.

The models show a ridge (a) about 5 million years ago (b) about 2 to 3 million years ago and (c) in the present.

Paleomagnetism (or palaeomagnetism in the United Kingdom) is the study of the record of the Earth's magnetic field in rocks, sediment, or archeological materials.

Two independently dated, high-resolution paleomagnetic records, one lacustrine and one archeological, record the passage across western North America of the same nondipole feature of the geomagnetic field during the time interval from A. Thank you for your interest in spreading the word about Science.

Although these sequences indicate that correlation between paleomagnetic and archeomagnetic records is feasible under certain conditions, differences between the records underscore the difficulty of dating accurately an archeological site by correlation of a single archeomagnetic direction with a secular variation curve.

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Both archeomagnetic ages using two individual dating methods generally overlapped with the radiocarbon age ranges for each sites.

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Magnetic stripes are the result of reversals of the Earth's field and seafloor spreading.

New oceanic crust is magnetized as it forms and then it moves away from the ridge in both directions.

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