Research
Seismic imaging reveals double slab tearing at a subduction–collision transition
Phys.org ·
The Brief
- An international research team used seismic imaging to identify two slab tears beneath the Zagros–Makran transition zone in southeastern Iran, near the Strait of Hormuz.
- The findings suggest the two tears formed through distinct geodynamic mechanisms.
- The source is a short summary; the full study details were not available in the provided text.
Why it matters
The study adds detail on how subducting slabs tear where an oceanic subduction zone transitions into continental collision, a process that shapes regional geodynamics and deformation.
Who’s affected
- geoscientists and seismologists studying subduction and continental collision
- researchers working on the tectonics of the Zagros and Makran regions
- #seismology
- #subduction
- #slab tearing
- #zagros
- #makran
- #geodynamics
An international research team has used seismic imaging to identify two slab tears beneath the Zagros–Makran transition zone located in southeastern Iran near the Strait of Hormuz. The findings suggest that the tears formed through distinct geodynamic mechanisms and may have…