Plate flexure and volcanism: Late Cenozoic tectonics of the Tabar-Lihir-Tanga-Feni alkalic province, New Ireland Basin, Papua New Guinea
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Cenozoic alkaline volcanoes, PNG, sit atop submarine ridges due to plate flexure.

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Alignment of the narrow 250 km long volcanic arc is orthogonal to ridges.

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Linear volcanic arc suggests ascent of alkaline magmas in arc-parallel fractures.

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Volcanism was localized at intersection of arc- and ridge-parallel structures.

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Unique volcano-tectonic history is key to origin of Earth's largest gold deposit.

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