Earth-prints repository, logo   DSpace

About DSpace Software
|earth-prints home page | roma library | bologna library | catania library | milano library | napoli library | palermo library
Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10165

Authors: Pavón-Carrasco, F. J.*
Osete, M. L.*
Campuzano, S. A.*
McIntosh, G.*
Martín-Hernández, F.*
Editors: Eppelbaum, L. V.; Telaviv Univ. (Israel)
Title: Recent developments in Archeomagnetism: the story of the Earth's past magnetic field
Other Titles: Recent developments in Archeomagnetism
Publisher: Nova Science Publishers
Issue Date: Sep-2015
ISBN: 978-1-63483-129-1
Keywords: Archeomagnetism
Paleomagnetism
Abstract: Since the pioneering studies in archeomagnetism in the second half of the 20th century, the number of archeomagnetic studies has increased exponentially. The huge density of archeomagnetic data collected during these years allows us to describe the past spatial and temporal evolution of the Earth’s magnetic field during the last millennia. Most of the data are located in the Northern Hemisphere, but currently, thanks to the strong effort of the paleomagnetic community, new collections of data are coming from the Southern Hemisphere, homogenizing the present database. Although the data distribution presents some epochs and locations where the data are still very scarce, they describe, to a greater or lesser degree of accuracy, the past behavior of the geomagnetic field. At regional scales, the use of archeomagnetic data permits the construction of paleosecular variation curves for the geomagnetic field elements: declination, inclination, and intensity. These curves describe the evolution of the elements at different times for the last millennia. During the last five years novel techniques, such as Bayesian statistics, bootstrap algorithms, or the Markov chain Monte Carlo method, have been applied to extract the most useful information from archeomagnetic data to build accurate and reliable curves. The accuracy of these curves can be exploited as a tool for archeomagnetic dating, assigning possible ages to archeological artifacts or volcanic lava flows with unknown age. At global scales, archeomagnetic data are jointly treated with other paleomagnetic data to generate continuous geomagnetic field models, reconstructing the past evolution of the geomagnetic field not only at the Earth’s surface, but also at the core-mantle boundary, shedding light on the past evolution of complex geodynamo processes.
Appears in Collections:04.05.08. Instruments and techniques
04.05.03. Global and regional models
Book chapters
04.05.07. Rock magnetism
04.05.06. Paleomagnetism
04.05.02. Geomagnetic field variations and reversals
04.05.05. Main geomagnetic field

Files in This Item:

File SizeFormatVisibility
Chapter. Pavón-Carrasco et al., 2015.pdf3.23 MBAdobe PDFonly authorized users View/Open


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.


Share this record
Del.icio.us

Citeulike

Connotea

Facebook

Stumble it!

reddit


 

Valid XHTML 1.0! ICT Support, development & maintenance are provided by CINECA. Powered on DSpace Software. CINECA