Paleomagnetic study of terrigenous rocks of the Uryuk Formation in the Southern Urals-Reference-Cited by-同舟云学术

Paleomagnetic study of terrigenous rocks of the Uryuk Formation in the Southern Urals

Published:2024-03-25 Issue:1 Volume: Page:103-112
ISSN:2619-0087
Container-title:Geologicheskii vestnik
language:
Short-container-title:Geol. vestn.

Author:

Parfiriev Nikita Petrovich¹,Danukalov Konstantin Nikolaevich¹,Golovanova Inessa Vladimirovna¹

Affiliation:

1. Institute of Geology — Subdivision of the Ufa Federal Research Centre of the Russian Academy of Sciences

Abstract

In order to obtain new paleomagnetic data on Vendian rocks in the Southern Urals, we studied the high-temperature magnetization component in sandstones of the Uryuk Formation, the carrier of which is hematite. The distinguished hematite vector in the collection of samples differs from the previously obtained intermediate-, intermediate-high-temperature magnetization component of magnetite, which is part of the same rocks. The average directions of the hematite component of magnetization of the Uryuk Formation were compared with the average directions of the overlying Basu Formation. The metachrony of the magnetite component and the synchrony of the hematite component are suggested.

Publisher

IG UFRC RAS

Link

http://geolvestnik.ru/File/2024/01/2024_01_08.pdf

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