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The Wetar back arc thrust belt in eastern Indonesia, spanning 350 km, results from the collision of Australia with the Indonesian island arc, featuring four main thrust faults. The geometry of the thrust belt is influenced by the irregular shape of the arc, leading to complex structural patterns and varying orientations of tectonic stress. This study utilizes seismic data to analyze the effects of arc geometry on the thrust belt structure and the implications for oblique convergence in the region.

Author

faris nauval

Language

EN