LOESS FORMATION IN THE LIGHT OF RECENT PALEOMAGNETIC DATA (GLOBAL REVIEW)

dc.contributor.author	Moszherin V.V.
dc.date.accessioned	2021-01-16T07:37:55Z
dc.date.available	2021-01-16T07:37:55Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=38726104
dc.identifier.citation	Geomorfologiya, 1999, , 3, 84-91
dc.identifier.issn	0435-4281
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/23186
dc.description.abstract	Loess rocks are widespread on the Earth. They occupy about 10% of global land area. Their thickness reaches up to 300 m in places and even more. Loess rocks differ in the different parts of the Earth. The 'warm' and the 'cold' loess rocks may be distinguished. They differ not only by conditions of their formation: the 'warm' loess rocks are older. The age of oldest loess according to magnetostratiraphic data is about 3.5 My. The accumulation rate of fine earth was estimated by paleomagnetic dating. Paleomagnetic method gives manifold possibilities for paleoclimate reconstructions.
dc.title	LOESS FORMATION IN THE LIGHT OF RECENT PALEOMAGNETIC DATA (GLOBAL REVIEW)
dc.type	Статья

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