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island arc |
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island arcCurved chain of volcanic islands. Island arcs are common in the Pacific where they ring the ocean on both sides; the Aleutian Islands off Alaska are an example. The volcanism that forms island arcs is a result of subduction of an oceanic plate beneath another plate, as evidenced by the presence of ocean trenches on the convex side of the arc, and the Benioff zone of high seismic activity beneath. Such island arcs are often later incorporated into continental margins during mountain-building episodes. |
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| The Kaputusan prospect is a typical Western Pacific island arc porphyry copper-gold system. A typical Island Arc type porphyry copper/ gold 'core' is now evident in the interpretation of the soil geochemical anomalies from the approximately 1km x 1km Kodu NW soil grid, weakening peripherally to a halo of molybdenum, lead and zinc geochemistry. The other half of the project area has a slightly deeper erosional level and is underlain by late Triassic to Cretaceous island arc intrusives |
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