Nd-, Sr-, O-isotopic and chemical evidence for a two-stage contamination history of mantle magma in the Central-Alpine Bergell intrusion

Author:

von Blanckenburg Friedhelm,Früh-Green Gretchen,Diethelm Karlheinz,Stille Peter

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference59 articles.

1. Arth JG, Barker F (1976) Rare-earth partitioning between hornblende and dacitic liquid and implications for the genesis of trondhjemitic-tonalitic magmas. Geology 4:534?536

2. Barth S, Oberli F, Meier M (1989) U-Th-Pb systematics of morphologically characterized zircon and allanite: a high-resolution isotopic study of the Alpine Rensen pluton (northern Italy). Earth Planet Sci Lett 95:235?254

3. Bernoulli D, Heitzmann P, Zingg A (1990) Central and southern Alps in southern Switzerland: tectonic evolution and first results of reflection seismics. In: Roure F, Heitzmann P, Polino R (eds) Deep structure of the Alps. Mém Soc géol France 156; Mém Soc géol suisse 1; Geol Soc Ital, Vol spec 1: 289?302

4. von Blanckenburg F (1990) Isotope geochemical and geochronological case studies of Alpine magmatism and metamorphism: the Bergell intrusion and Tauern Window. PhD dissertation ETH Zürich

5. Chen C-H, Shieh Y-N, Lee T, Chen C-H, Mertzman SA (1990) Nd-Sr-O isotopic evidence for source contamination and an unusual mantle component under Luzon Arc. Geochim Cosmochim Acta 54:2473?2483

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