Syn‐rift hydrothermal circulation in the Mesozoic carbonates of the western Adriatic continental palaeomargin (Western Southalpine Domain, NW Italy)

Author:

Barale L.1,Bertok C.2ORCID,d’Atri A.12,Mantovani A.2,Martire L.2,Agostini S.3ORCID,Bernasconi S. M.4ORCID,Gerdes A.5,Ferrando S.2

Affiliation:

1. Torino Unit National Research Council of ItalyInstitute of Geosciences and Earth Resources Torino Italy

2. Department of Earth Sciences University of Torino Torino Italy

3. National Research Council of ItalyInstitute of Geosciences and Earth Resources Pisa Italy

4. Department of Earth Sciences ETH Zurich Zurich Switzerland

5. Department of Geosciences Goethe University Frankfurt Frankfurt am Main Germany

Funder

Compagnia di San Paolo

Publisher

Wiley

Subject

Geology

Reference92 articles.

1. Zur Stratigraphie, Petrographie und zum tektonischen Aufbau der Canavese‐Zone und ihrer Lage zum Insubrischen Linie zwischen Biella und Cuorgné (Norditalien);Ahrendt H.;Göttinger Arbeiten Zur Geologie Und Paläontologie,1972

2. Baggio P.(1965).Caratteri stratigrafici e strutturali del Canavese s.s. nella zona di Montalto Dora. Mem. Ist. Geol. Mineral. Univ. Padova 25 1–25.

3. U‐Pb dating and geochemical constraints to Early Cretaceous hydrothermal dolomitization in the Provençal Domain (Maritime Alps, NW Italy–SE France);Barale L.;Ofioliti,2021

4. Very hot, very shallow hydrothermal dolomitization: An example from the Maritime Alps (north-west Italy-south-east France)

5. A crustal‐scale view at rift localization along the fossil Adriatic margin of the Alpine Tethys preserved in NW Italy

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