Deeply subducted continental fragments - Part 2: Insight from petrochronology in the central Sesia Zone (western Italian Alps)

Subducted continental terranes commonly comprise an assembly of subunits that reflect the different tectono-metamorphic histories they experienced in the subduction zone. Our challenge is to unravel how, when, and in which part of the subduction zone these subunits were juxtaposed. Petrochronology offers powerful tools to decipher pressure-temperature-time (P-T-t) histories of metamorphic rocks that preserve a record of several stages of transformation. A major issue is that the driving forces for re-equilibration at high pressure are not well understood. For example, continental granulite terrains subducted to mantle depths frequently show only partial and localized eclogitization. The Sesia Zone (NW Italy) is exceptional because it comprises several continental subunits in which eclogitic rocks predominate and high-pressure (HP) assemblages almost completely replaced the Permian granulite protoliths. This field-based study comprises both main complexes of the Sesia terrane, covering some of the recently recognized tectonic subunits involved in its assembly; hence our data constrain the HP tectonics that formed the Sesia Zone. We used a petrochronological approach consisting of petrographic and microstructural analysis linked with thermodynamic modelling and U-Th-Pb age dating to reconstruct the P-T-t trajectories of these tectonic subunits. Our study documents when and under what conditions re-equilibration took place. Results constrain the main stages of mineral growth and deformation, associated with fluid influx that occurred in the subduction channel. In the Internal Complex (IC), pulses of fluid percolated at eclogite facies conditions between 77 and 55ĝ€Ma with the HP conditions reaching ĝ1/4 ĝ€-2ĝ€-GPa and 600-670ĝ€-°C. By contrast, the External Complex (EC) records a lower pressure peak of ĝ1/4 ĝ€-0.8ĝ€-GPa for 500ĝ€-°C at ĝ1/4 ĝ€-63ĝ€-Ma. The juxtaposition of the two complexes occurred during exhumation, probably at ĝ1/4 ĝ€-0.8ĝ€-GPa and 350ĝ€-°C; the timing is constrained between 46 and 38ĝ€-Ma. Mean vertical exhumation velocities are constrained between 0.9 and 5.1ĝ€-mmĝ€-yearĝ'1 for the IC, up to its juxtaposition with the EC. Exhumation to the surface occurred before 32ĝ€-Ma, as constrained by the overlying Biella Volcanic Suite, at a mean vertical velocity between 1.6 and 4ĝ€-mmĝ€-yearĝ'1. These findings constrain the processes responsible for the assembly and exhumation of HP continental subunits, thus adding to our understanding of how continental terranes behave during subduction.