Untersuchungen an Kugelgraniten aus den Zillertaler Alpen (Tirol, Österreich)

P. K. Hörmann; K. Mignon; G. Morteani; P. Rudan

doi:10.1007/BF01134166

Untersuchungen an Kugelgraniten aus den Zillertaler Alpen (Tirol, Österreich)

Translated title of the contribution: Investigations on orbiculitic granites from the Zillertal Alps (Tyrol, Austria)

P. K. Hörmann, K. Mignon, G. Morteani, P. Rudan

Christian-Albrechts-University of Kiel

Research output: Contribution to journal › Article › peer-review

Abstract

A new occurence of orbiculitic rocks from the Western Zillertal Alps is investigated. The orbicules consist of a core and a shell. The core is poor in potassium feldspar and rich in quartz and biotite. The shell consists mainly of potassium feldspar. Three chemical analyses. The shell consists mainly analyses, and thirty-one modal analyses were carried out. It is concluded that the orbicules have been derived from xenoliths by a partial melting process.

Translated title of the contribution	Investigations on orbiculitic granites from the Zillertal Alps (Tyrol, Austria)
Original language	German
Pages (from-to)	156-172
Number of pages	17
Journal	Tschermaks Mineralogische und Petrographische Mitteilungen
Volume	16
Issue number	3
DOIs	https://doi.org/10.1007/BF01134166
State	Published - Sep 1971
Externally published	Yes

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abstract = "A new occurence of orbiculitic rocks from the Western Zillertal Alps is investigated. The orbicules consist of a core and a shell. The core is poor in potassium feldspar and rich in quartz and biotite. The shell consists mainly of potassium feldspar. Three chemical analyses. The shell consists mainly analyses, and thirty-one modal analyses were carried out. It is concluded that the orbicules have been derived from xenoliths by a partial melting process.",

author = "H{\"o}rmann, {P. K.} and K. Mignon and G. Morteani and P. Rudan",

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AU - Rudan, P.

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AB - A new occurence of orbiculitic rocks from the Western Zillertal Alps is investigated. The orbicules consist of a core and a shell. The core is poor in potassium feldspar and rich in quartz and biotite. The shell consists mainly of potassium feldspar. Three chemical analyses. The shell consists mainly analyses, and thirty-one modal analyses were carried out. It is concluded that the orbicules have been derived from xenoliths by a partial melting process.

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ER -

Untersuchungen an Kugelgraniten aus den Zillertaler Alpen (Tirol, Österreich)

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