Metamorphic evolution of the Sesia-Lanzo Zone, Western Alps: time constraints from multi-system geochronology

The Sesia-Lanzo Zone is a polymetamorphic unit containing Hercynian granulite relics overprinted by eclogite and greenschist facies metamorphism and deformation during the Alpine orogeny. Metamorphic evolution is discussed.

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Veröffentlicht in:Contributions to mineralogy and petrology 1996-12, Vol.126 (1-2), p.152-168
Hauptverfasser: Inger, S., Ramsbotham, W., Cliff, R. A., Rex, D. C.
Format: Artikel
Sprache:eng
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Zusammenfassung:The Sesia-Lanzo Zone is a polymetamorphic unit containing Hercynian granulite relics overprinted by eclogite and greenschist facies metamorphism and deformation during the Alpine orogeny. Metamorphic evolution is discussed.
ISSN:0010-7999
1432-0967
DOI:10.1007/s004100050241