CHLORINE-36 EVIDENCE FOR THE MONO LAKE EVENT IN THE SUMMIT GRIP ICE CORE

dc.contributor.author	Wagner G.
dc.contributor.author	Beer J.
dc.contributor.author	Laj C.
dc.contributor.author	Kissel C.
dc.contributor.author	Masarik J.
dc.contributor.author	Muscheler R.
dc.contributor.author	Synal H.A.
dc.date.accessioned	2021-01-24T05:12:18Z
dc.date.available	2021-01-24T05:12:18Z
dc.date.issued	2000
dc.identifier	https://www.elibrary.ru/item.asp?id=367735
dc.identifier.citation	Earth and Planetary Science Letters, 2000, 181, 1-2, 1-6
dc.identifier.issn	0012-821X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/23642
dc.description.abstract	A distinct peak has been discovered in the 36Cl data from the GRIP ice core between the Dansgaard Oeschger (D-O) events 6 and 7 at approximately 32 kyr BP. This peak can be attributed to a minimum of the geomagnetic dipole field associated with the Mono Lake event. Since the 36Cl peak reflects a higher production rate of all cosmogenic radionuclides, it has an impact on the 14C dating of the last ice age. Furthermore, it provides an additional time marker similar to a peak found earlier corresponding to the Laschamp event at approximately 39 kyr BP.
dc.subject	CL-36
dc.subject	MAGNETIC FIELD
dc.subject	PALEOMAGNETISM
dc.subject	COSMOGENIC ELEMENTS
dc.subject	RADIOACTIVE ELEMENTS
dc.title	CHLORINE-36 EVIDENCE FOR THE MONO LAKE EVENT IN THE SUMMIT GRIP ICE CORE
dc.type	Статья

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