Dissemin is shutting down on January 1st, 2025

Links

Tools

Export citation

Search in Google Scholar

Connection of Neogene Basin Formation, Magmatism and Cooling of Metamorphics in Ne Slovenia

This paper is available in a repository.
This paper is available in a repository.

Full text: Download

Question mark in circle
Preprint: policy unknown
Question mark in circle
Postprint: policy unknown
Question mark in circle
Published version: policy unknown

Abstract

The Mura-Zala basin was born due to crustal extension between ~18 and~13 Ma. Extension resulted in half grabens and fastly subsiding basin floor. However, metamorphic rocks and Neogene magmatites were exhumed synchronously at the western basin margin, probably along low-angle ductile shear zones. After a late Miocene thermal phase and a Pliocene folding of the southernmost half grabens, all the area suffered a uniform, ~30º counterclockwise rotation.