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Sunda-Java SZI Events

Sunda-Java subduction zone initiation

The Sunda-Java SZI event likely re-initiated subduction at Sundaland’s southern margin between 60–40 Ma. The evolving subduction zone’s history includes earlier accretion of the Woyla arc, a hiatus in subduction, and evidence from seismic tomography suggesting the current slab’s depth aligns with historical models, indicating significant tectonic interactions over time.