2022
DOI: 10.1002/essoar.10511199.1
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Global constraints on intermediate-depth intraslab stresses from slab geometries and mechanisms of double seismic zone earthquakes

Christian Sippl
1
,
Armin Dielforder
2
,
Timm John
3
et al.

Abstract: Subducting slabs of oceanic lithosphere are subject to forces such as slab pull, ridge push, or mantle drag that control the state of stress within the slab (e.g.,

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