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Emersion of Distal Domains in Advanced Stages of Continental Rifting Explained by Asynchronous Crust and Mantle Necking.
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- Geochemistry, Geophysics, Geosystems: G3, 2019, v. 20, n. 8, p. 3821, doi. 10.1029/2019GC008357
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Shallow-burial hydrothermal dolomitization: lessons from the Western and Central Alps.
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- Geophysical Research Abstracts, 2018, v. 20, p. 8338
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Tectono‐thermal Evolution of a Distal Rifted Margin: Constraints From the Calizzano Massif (Prepiedmont‐Briançonnais Domain, Ligurian Alps).
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- Tectonics, 2017, v. 36, n. 12, p. 3209, doi. 10.1002/2017TC004634
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Architecture of the Distal Piedmont-Ligurian Rifted Margin in NW Italy: Hints for a Flip of the Rift System Polarity.
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- Tectonics, 2017, v. 36, n. 11, p. 2388, doi. 10.1002/2017TC004561
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Tracing the thermal evolution of the Corsican lower crust during Tethyan rifting.
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- Tectonics, 2016, v. 35, n. 10, p. 2439, doi. 10.1002/2016TC004178
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A crustal-scale view at rift localization along the fossil Adriatic margin of the Alpine Tethys preserved in NW Italy.
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- Tectonics, 2015, v. 34, n. 9, p. 1927, doi. 10.1002/2015TC003973
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Unravelling the interaction between tectonic and sedimentary processes during lithospheric thinning in the Alpine Tethys margins.
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- International Journal of Earth Sciences, 2010, v. 99, p. 75, doi. 10.1007/s00531-010-0566-6
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The role of rift-inherited hyper-extension in Alpine-type orogens.
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- Terra Nova, 2014, v. 26, n. 5, p. 347, doi. 10.1111/ter.12104
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CAN THE SCALE OF OBSERVATION HIDE COMPLEXITIES IN THE DEFORMATION HISTORY OF A TERRANE? AN EXAMPLE FROM THE BALMUCCIA PERIDOTITE MASSIF, IVREA ZONE (NW ITALY).
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- Ofioliti, 2021, v. 46, n. 2, p. 107, doi. 10.4454/ofioliti.v46i2.541
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