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 |
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Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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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. |
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ISSN: | 0010-7999 1432-0967 |
DOI: | 10.1007/s004100050241 |