HIGHLIGHTS
SUMMARY
To observe the stress field evolution with depth (Fig 2) and the associated distribution of focal mechanisms, the authors divided them into 10-km thick depth intervals. At depths > 140 km, where the dehydration of the 10-Å phase (or other minerals such as phase A) is characterized by a positive Clapeyron s lope9, focal mechanisms indicate a compressional stress field and R decreases. The limited delamination of the Carpathian lithosphere20 that induced slab v erticalization4,62 has resulted in a relatively simple slab geometry, which helps the visualization of the potential impact of dehydration . . .
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