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  • Print publication year: 2017
  • Online publication date: May 2017

6 - Palaeomagnetic Geochronology of Quaternary Sequences in the Levant1

from Part I: - The Evolution of Current Landscapes and Basins
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Summary

Paleomagnetic dating methods are based on comparing magnetic information from materials or sequences whose ages are unknown with a geomagnetic chronological reference frame. The global Quaternary geomagnetic chronology is continuously updated and includes at the moment 10 polarity reversals and at least 18 validated geomagnetic excursions that serve as detectable markers for sedimentary and volcanic sequences. In addition, short-term secular geomagnetic variations of the Holocene provide the basis for a promising method for dating young materials. In this chapter we review the principles underlying paleomagnetic dating methods with emphasis on Quaternary rocks, sediments, and archaeological materials. We summarize a number of successful applications of paleomagnetic chronology in Quaternary research in the Levant, and present insight into future prospects of Quaternary paleomagnetism.
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