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(Article of periodic en Anglais - 2012)

Document title

Palaeomagnetic investigation of Cenozoic volcanic rocks bordering the North Anatolian Fault Zone, Reşadiye and Koyulhisar Districts, central-east Anatolia, Turkey

Authors(s) and Affiliation(s)

KOÇBULUT F. (1) ;
(1) Dept. of Geology, Cumhuriyet Univ., Sivas, TURQUIE

Abstract

A palaeomagnetic study is reported from the lavas of Eocene, Miocene and Pliocene age cropping out immediately to the north of the North Anatolian Fault Zone (NAFZ) in the Reşadiye–Mesudiye region of central-eastern Anatolia. Rock magnetic investigations identify a high percentage of multi-domained magnetite as the dominant ferromagnet in these rocks. Thirty of 37 units yielded acceptable groupings of characteristic magnetisation directions. An earlier study indicated small anticlockwise crustal block rotation in this region since Upper Cretaceous times. This study indicates that this was overtaken by clockwise rotation in Eocene times. Results from later Miocene and Pliocene volcanic rocks indicate that no significant tectonic rotation has occurred in the north of the NAFZ in Neogene times. This contrasts with rotations in the weaker crust comprising the Anatolian collage south of the NAFZ, where differential and sometimes large anticlockwise rotations occurred during the latter part of the Neogene

Source

Article of periodic

published at : Geodinamica acta / ISSN 0985-3111

Editor : Taylor & Francis, Abingdon - ROYAUME-UNI (1987)

Millesime : 2012, vol. 25, no1-2 [pp. 26-37]

Bibliographic references : 2 p.

Collation : 6 fig., 4 tabl.

Language

Anglais

INIST-CNRS, Cote INIST : 21088

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.1080/09853111.2013.838061

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2014
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