Petrology of Păuliş granites (Apuseni Mts., Romania)

Pál Molnár Elemér and András Eduárd and Kassay Zsombor and Buda György and Batki Anikó: Petrology of Păuliş granites (Apuseni Mts., Romania). In: Acta mineralogica-petrographica, (48). pp. 33-41. (2008)

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Abstract

This paper presents new data of the highly evolved part of the Highis Granitoid Suite. Two types of texture represent the suite: equigranular, medium-grained leucogranites and aplite veins. Main rock forming minerals are quartz, orthoclase, microcline, plagioclase feldspar, biotite and muscovite. Based on geochemical investigations which were performed on both selected mineral phases and whole rock composition the Highi$ Granitoids from P5uli§ are S-type, felsic-peraluminous alkali granites, with alkali-calcic character, formed in post-collisional (postorogenic) tectonical setting, mainly from metasedimentary source.

Item Type: Article
Heading title: Articles
Journal or Publication Title: Acta mineralogica-petrographica
Date: 2008
Volume: 48
ISSN: 0365-8066
Page Range: pp. 33-41
Language: English
Publisher: Department of Mineralogy, Geochemistry and Petrology, University of Szeged
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39430/
Uncontrolled Keywords: Földtan, Ásványtan, Kőzettan
Additional Information: Bibliogr.: p. 40-41. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:24
Last Modified: 2022. Aug. 26. 08:26
URI: http://acta.bibl.u-szeged.hu/id/eprint/25150

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