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Journal of Petrology | Volume 43 | Number 9 | Pages 1783-1786 | 2002
© Oxford University Press 2002

Cadomian Lower-crustal Contributions to Variscan Granite Petrogenesis (South Bohemian Pluton, Austria): a Reply

U. S. KLÖTZLI1,*, F. KOLLER2, S. SCHARBERT3 and V. HÖCK4

1LABORATORY FOR GEOCHRONOLOGY, INSTITUTE OF GEOLOGY, UNIVERSITY OF VIENNA, GEOZENTRUM, ALTHANSTRASSE 14, A-1090 VIENNA, AUSTRIA
2INSTITUTE OF PETROLOGY, UNIVERSITY OF VIENNA, GEOZENTRUM, ALTHANSTRASSE 14, A-1090 VIENNA, AUSTRIA
3GEOLOGICAL SURVEY OF AUSTRIA, RASUMOFSKYGASSE 23, A-1030 VIENNA, AUSTRIA
4INSTITUTE OF GEOLOGY AND PALAEONTOLOGY, UNIVERSITY OF SALZBURG, HELLBRUNNERSTRASSE 34, A-5020 SALZBURG, AUSTRIA

Received February 5, 2002; Revised typescript accepted March 14, 2002

The first 150 words of the full text of this article appear below.


   PREFACE
 
The comment by Finger & Clemens (2002) nicely confirms the statement in the introduction of our paper (Klötzli et al., 2001) on p. 1622: ‘Unravelling the origin of a given granite still requires a major analytical effort and commonly ends in some contradictory results’. Finger & Clemens raise a number of issues, both minor and major. We will discuss all of them, as far as they are relevant to the subject. We will start with the problem of nomenclature. After that we will address the problem of remnants of an old crustal component versus a cumulate origin and the problem of the age of the crustal remnants.


   PETROLOGY
 
Opx- and cpx-bearing Weinsberg type granitoid rocks are widespread in an area of ~15–20 km2 surrounding the villages of Sarleinsbach, Sprinzenstein and Arnreit in the Southern Bohemian Massif (Klötzli et al., 2001, figs 1 and 2). This . . . [Full Text of this Article]


   GEOCHRONOLOGY
 

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