Fabrizio Balsamo is Assocaite Professor at the
Department of Chemistry, Life Sciences and Environmental Sustainability at the
University of Parma, Italy. He received his PhD in Geodynamics from the
University of Roma Tre, Italy in 2006. From 2006 to 2011, he was a Post-doc at
the Department of Geology, University of Rome Tre, Italy. From 2011 to 2017, he
was also a Post-doc and research fellow at the Department of Physics and Earth
Sciences, University of Parma, Italy. In 2009, he was a visiting researcher at
Universidade Federal do Rio Grande do Norte (UFRN), Brazil. From 2017 to 2019
assistant professor at the Department of Chemistry, Life Sciences and
Environmental Sustainability, University of Parma, Italy. His primary interests
concern structural geology and tectonics, with focus on the quantitative
analysis of brittle deformation at different scales (micro to regional) aimed
to understand (1) the structural architecture of fault systems, (2)
petrophysical properties of fault rocks, (3) signature of seismic vs aseismic
slip in shallow sediments, and (4) interplay between deformation and fluid
flow.
Fabrizio Balsamo is Assocaite Professor at the
Department of Chemistry, Life Sciences and Environmental Sustainability at the
University of Parma, Italy. He received his PhD in Geodynamics from the
University of Roma Tre, Italy in 2006. From 2006 to 2011, he was a Post-doc at
the Department of Geology, University of Rome Tre, Italy. From 2011 to 2017, he
was also a Post-doc and research fellow at the Department of Physics and Earth
Sciences, University of Parma, Italy. In 2009, he was a visiting researcher at
Universidade Federal do Rio Grande do Norte (UFRN), Brazil. From 2017 to 2019
assistant professor at the Department of Chemistry, Life Sciences and
Environmental Sustainability, University of Parma, Italy. His primary interests
concern structural geology and tectonics, with focus on the quantitative
analysis of brittle deformation at different scales (micro to regional) aimed
to understand (1) the structural architecture of fault systems, (2)
petrophysical properties of fault rocks, (3) signature of seismic vs aseismic
slip in shallow sediments, and (4) interplay between deformation and fluid
flow.