REMOTE DETERMINATION OF THE DIRECTION TO THE GEOMAGNETIC POLE IN PAST EPOCHS

dc.contributor.author	Yakupov V.S.
dc.contributor.author	Yakupov M.V.
dc.contributor.author	Yakupov S.V.
dc.date.accessioned	2024-10-27T02:28:48Z
dc.date.available	2024-10-27T02:28:48Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13518440
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1470-1472
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46269
dc.description.abstract	The possibility of remote detection of the direction to the geomagnetic pole in past epochs is considered on the basis of using the Faraday effect in the process of radar sounding and recording of the magnetic component of reflected signals. The results of paleomagnetic investigations made it possible to distinguish the drift of continents and trajectories of their motion in past epochs. These results facilitated significantly the development and formation of the modern paradigm of geology: tectonics of lithospheric plates.
dc.title	REMOTE DETERMINATION OF THE DIRECTION TO THE GEOMAGNETIC POLE IN PAST EPOCHS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090303

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