Structure of the lithosphere beneath the Eastern Alps (southern sector of the TRANSALP transect)

Author:

Castellarin Alberto,Nicolich Rinaldo,Fantoni Roberto,Cantelli Luigi,Sella Mattia,Selli Luigi

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference121 articles.

1. Calc-alkaline basic to silicic rocks suites from the Late Hercynian Atesina–Cima d'Asta volcano–plutonic complex (Southern Alps, N Italy): evidences for primary magmatic and hydrothermal alteration processes;Barth;N. Jb. Miner. Abh.,1994

2. The evolution of a calc-alkaline basic to silicic magma system: geochemical and Rb–Sr, Sm–Nd, and O18/O16 isotopic evidence from the Late Hercynian Atesina–Cima d'Asta volcano–plutonic complex, Northern Italy;Barth;Geochim. Cosmochim. Acta,1993

3. Crustal scale extension in a convergent orogene: the Sterzing–Steinach mylonite zone in the Eastern Alps;Behrmann;Geoynamica Acta,1988

4. Evolution of continental margins in the Alps;Bernoulli;Schweiz. Mineral. Petrogr. Mitt.,1979

5. Upper crustal style shortening and deformation age in the Alps along the southern sector of the TRANSALP profile;Bertelli,2003

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