Dehydration-induced earthquakes identified in a subducted oceanic slab beneath Vrancea, Romania.

ABSTRACT: Vrancea, Eastern Romania, presents a significant intermediate-depth seismicity, between 60 and 170 km depth, i.e. pressures from 2 to 6.5 GPa. A debate has been lasting for decades regarding the nature of the seismic volume, which could correspond to the remnant of a subducted slab of Tethyan lithosphere or a delamination of the Carpathians lithosphere. Here we compile the entire seismicity dataset (≈ 10,000 events with 2 ≤ Mw ≤ 7.9) beneath Vrancea for P > 0.55 GPa (> 20 km) since 1940 and estimate the pressure and temperature associated with each hypocenter. We infer the pressure and temperature, respectively, from a depth-pressure conversion and from the most recent tomography-based thermal model. Pressure-temperature diagrams show to what extent these hypocentral conditions match the t

SUBMITTER: Ferrand TP 

PROVIDER: S-EPMC8119720 | biostudies-literature | 2021 May

REPOSITORIES: biostudies-literature