The Fina Nagu Volcanic Complex: Unusual Submarine Arc Volcanism in the Rapidly Deforming Southern Mariana Margin
In the Mariana convergent margin, large arc volcanoes disappear south of Guam even though the Pacific plate continues to subduct and instead, small cones scatter on the seafloor. These small cones could form either due to decompression melting accompanying back-arc extension or flux melting, as expected for arc volcanoes, or as a result of both processes.

