New Paleomagnetic Data on the Devonian–Early Carboniferous Strata in Tuva

New paleomagnetic data on the Devonian and Early Carboniferous rocks in Tuva have been obtained. Component analysis of magnetization has been carried out. Coordinates of the paleomagnetic poles have been calculated: Φ = 53.8, Λ = 141.7, and A95 = 9.6 (Early Carboniferous); Φ = 3.7, Λ = 139.8, and A9...

Full description

Saved in:
Bibliographic Details
Published inDoklady earth sciences Vol. 491; no. 1; pp. 121 - 126
Main Authors Kovalenko, D. V., Buzina, M. V., Lobanov, K. V.
Format Journal Article
LanguageEnglish
Published Moscow Pleiades Publishing 01.03.2020
Springer
Springer Nature B.V
Subjects
Analysis
Carboniferous
Devonian
Earth and Environmental Science
Earth Sciences
Geology
Magnetism
Magnetization
Palaeomagnetism
Paleomagnetism
Rock
Rocks
Strata
Tuva
shear
rotation in the horizontal plane
мagnetization
deformations
magnetization declination
magnetization inclination
Online AccessGet full text

Cover

More Information
Summary:New paleomagnetic data on the Devonian and Early Carboniferous rocks in Tuva have been obtained. Component analysis of magnetization has been carried out. Coordinates of the paleomagnetic poles have been calculated: Φ = 53.8, Λ = 141.7, and A95 = 9.6 (Early Carboniferous); Φ = 3.7, Λ = 139.8, and A95 = 9.3 (beginning of the Late Devonian). The Early Carboniferous rocks were formed in the latitude range of 51°–70.5° N; rocks in the upper part of the Upper Devonian strata, 42°–68° N; and the lower part of the Upper Devonian strata, 21°–36° N. The large geological blocks of Tuva likely rotated in the horizontal plane due to the action of high-amplitude shears.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X20030101