Skip to main content
Book Chapter

The Habach-Formation and the Zentralgneis — A Key in Understanding the Palaeozoic Evolution of the Tauern Window (Eastern Alps)

  • Höck V
Springer Berlin Heidelberg, (1993), 361-374
DOI: 10.1007/978-3-642-84640-3_22
N/ACitations
Citations of this article
3Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The pre-Permian Habach formation is a complicated metamorphosed sequence of magmatic and sedimentary rocks within the Tauern window. It can be separated into three subunits:1.Ophiolites including the Basisamphibolit;2.An island arc volcanic sequence;3.The Eiser sequence (Biotitporphyroblastenschiefer).

Cite

CITATION STYLE

APA

Höck, V. (1993). The Habach-Formation and the Zentralgneis — A Key in Understanding the Palaeozoic Evolution of the Tauern Window (Eastern Alps). In Pre-Mesozoic Geology in the Alps (pp. 361–374). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-84640-3_22

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free