Oceanic-continental subduction zones is the geologic setting where andesite magmas could be found.
At convergent plate boundaries, the oceanic lithosphere—the outer layer of the Earth made up of the crust and upper mantle—is subducted until its edge is positioned beneath the edge of the continental plate or another oceanic plate. At these locations, granitic, or rhyolitic, magmas as well as andesitic magmas are produced. Andesitic/rhyolitic magma creates stratovolcanoes, often known as composite volcanoes.
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