THE MAGNETOSTRATIGRAPHY AND A 1780 MA PALAEOMAGNETIC POLE FROM THE RED SANDSTONES OF THE VAZHINKA RIVER SECTION, KARELIA, RUSSIA

dc.contributor.author	Pisarevsky S.A.
dc.contributor.author	Sokolov S.J.
dc.date.accessioned	2021-02-25T05:13:22Z
dc.date.available	2021-02-25T05:13:22Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13386143
dc.identifier.citation	Geophysical Journal International, 2001, 146, 2, 531-538
dc.identifier.issn	0956-540X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/25723
dc.description.abstract	A palaeomagnetic study of the Vepsian sandstones of the upper part of the Shoksha Formation has revealed a stable remanence. Rock magnetic and mineralogical studies suggest diagenetic haematite as the main carrier of this remanence. Two magnetic polarities with a regular stratigraphic zonation have been found. The reversal test is positive. The tilt-corrected palaeomagnetic direction is: N = 36, D = 354.3°, I = 21.6°, k = 22.3, 95 = 5.2°. The corresponding palaeomagnetic pole of 39.7°N, 221.1°E (Dp = 2.9°, Dm = 5.5°) is proposed as a ‘key pole’ for 1790–1770 Ma for Fennoscandia.
dc.title	THE MAGNETOSTRATIGRAPHY AND A 1780 MA PALAEOMAGNETIC POLE FROM THE RED SANDSTONES OF THE VAZHINKA RIVER SECTION, KARELIA, RUSSIA
dc.type	Статья

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