Multiple zircon growth and recrystallization during polyphase Late Carboniferous to Triassic metamorphism in granulites of the Ivrea Zone (Southern Alps): an ion microprobe (SHRIMP) study

A study examined zircons from a granulite of the Val Sesia and Val Mastallone area of the Ivrea Zone in the Southern Alps. The morphology of the zircons and the chemistry of the rock suggest that the magma was calcalkaline.

Saved in:
Bibliographic Details
Published inContributions to mineralogy and petrology Vol. 122; no. 4; pp. 337 - 358
Main Authors Vavra, G., Gebauer, Dieter, Schmid, Rolf, Compston, William
Format Journal Article
LanguageEnglish
Published Heidelberg Springer Nature B.V 01.01.1996
Subjects
Carboniferous
Crystallography
Crystals
Geology
Metamorphism
Mineralogy
Petrology
Triassic
Online AccessGet full text
ISSN0010-7999
1432-0967
DOI10.1007/s004100050132

Cover

More Information
Summary:A study examined zircons from a granulite of the Val Sesia and Val Mastallone area of the Ivrea Zone in the Southern Alps. The morphology of the zircons and the chemistry of the rock suggest that the magma was calcalkaline.
Bibliography:SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 14
ISSN:0010-7999
1432-0967
DOI:10.1007/s004100050132