Evidence for excess argon during high pressure metamorphism in the dora maira massif (Western Alps, Italy), using an ultra-violet laser ablation microprobe 40Ar-39Ar technique

Author:

Arnaud N. O.,Kelley S. P.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference32 articles.

1. Biino G, Compagnoni R, Lombardo B, Sandrone R (1988) The pyrope-coesite-phengite-kyanite-talc whiteschist of case Parigi, southern Dora Maira massif. In: Piccardo (ed) High pressure eclogitic reequilibration in the western Alps. IGCP No235, Genova, pp

2. Biino GG, Compagnoni R (1992) Very high pressure metamorphism of the Brossasco coronite metagranite, southern Dora Maira massif, western Alps, Schweiz Mineral Petrogr Mitt 72:347–363

3. Bowtell SA, Cliff RA, Barnicoat AC (1994) Sm-Nd isotopic evidence on the age of eclogitization in the Zermatt-Saas ophiolite. J Metamorphic Geol 12:187–196

4. Chopin C (1984) Coesite and pure pyrope in high grade blueschists of the western Alps: a first record and some consequences. Contrib Mineral Petrol 86:107–118

5. Chopin C, Maluski H (1980) 40Ar/39Ar dating of high pressure metamorphic micas from the gran Paradiso area (western Alps): evidence against the blocking temperature concept. Contrib Mineral Petrol 74: 109–122

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