Detailed Jaramillo field reversals recorded in lake sediments from Armenia – Lower mantle influence on the magnetic field revisited

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Detailed Jaramillo field reversals recorded in lake sediments from Armenia – Lower mantle influence on the magnetic field revisited

While it is well established that the Earth's magnetic field is generated by a self sustaining dynamo that reversed its polarity at irregular intervals in the geological past, the very mechanisms causing field reversals remain obscure. Paleomagnetic reconstructions of polarity transitions have...

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Bibliographic Details
Main Authors:	Kirscher, Uwe, Winklhofer, M., Hackl, M., Bachtadse, V.
Format:	Journal Article
Published:	Elsevier BV 2018
Online Access:	http://hdl.handle.net/20.500.11937/60093

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