The geodynamic evolution of the Italian South Alpine basement from the Ediacaran to the Carboniferous: Was the South Alpine terrane part of the peri-Gondwana arc-forming terranes?-Reference-Cited by-同舟云学术

The geodynamic evolution of the Italian South Alpine basement from the Ediacaran to the Carboniferous: Was the South Alpine terrane part of the peri-Gondwana arc-forming terranes?

Published:2019-01 Issue: Volume:65 Page:17-30
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Arboit F.,Chew D.,Visoná D.,Massironi M.,Sciascia F.,Benedetti G.,Rodani S.

Funder

Irish Research Council

Science Foundation Ireland

Publisher

Elsevier BV

Subject

Geology

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1. Permian thermally-induced shear of the Cossato-Mergozzo-Brissago shear zone in the W-Southalpine basement, Italy: new petrological, geochemical and U–Pb geochronological constraints from the amphibolite-facies units of the Strona Ceneri Border Zone;International Journal of Earth Sciences;2024-06-21

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5. Cadomian to Cenerian accretionary orogenic processes in the Alpine basement: the detrital zircon archive;International Journal of Earth Sciences;2023-03-23