@article{fdi:010090549,
  title = {{U}-{P}b carbonate dating reveals long-lived activity of proximal margin extensional faults during the {A}lpine {T}ethys rifting},
  author = {{R}occa, {M}. and {Z}anchetta, {S}. and {G}asparrini, {M}. and {M}angenot, {X}. and {B}erra, {F}. and {D}eschamps, {P}ierre and {G}uihou, {A}. and {Z}anchi, {A}.},
  editor = {},
  language = {{ENG}},
  abstract = {{S}yn-rift extensional faults play a significant role during the early stage of rifting. {C}onstraining the age of faulting, and how and when deformation shifts from the proximal to the distal margin areas, is crucial for the reconstruction of the rifting process. {P}revious assessments of the structural and temporal evolution of rift-related faults of the {A}dria proximal margin have primarily relied on indirect biostratigraphic evidence. {A}dditionally, the majority of rift-related faults underwent tectonic inversion during the {A}lpine orogeny. {I}n this study, in-situ {U}-{P}b geochronology was applied on syn-kinematic calcites to unravel the activity of the {A}mora {F}ault, a remarkable example of a {J}urassic growth fault unaffected by the {A}lpine orogeny. {T}he obtained ages, spanning from {H}ettangian to {C}allovian, extend the {AF} activity beyond the previously established {E}arly {J}urassic time. {T}his chrono-structural model has significant implications on the role of major extensional faults in focusing deformation throughout the rift system's evolution.},
  keywords = {{A}lpine {T}ethys ; extensional faults ; {J}urassic rifting ; {S}outhern {A}lps ; {U}-{P}b ; carbonate dating ; {ITALIE} ; {ALPES}},
  booktitle = {},
  journal = {{T}erra {N}ova},
  volume = {36},
  numero = {5},
  pages = {347--357},
  ISSN = {0954-4879},
  year = {2024},
  DOI = {10.1111/ter.12717},
  URL = {https://www.documentation.ird.fr/hor/fdi:010090549},
}