Fragments of the Olyutor island arc formed in the Pacific during the Late Cretaceous–Paleogene [1, 8]. At the time they were located far away (about 2000 km) from the Eurasian continental margin [2, 3]; at present, this is a part of the Olyutor–Kamchatka fold region. In the modern structure, Cretace...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.567.1710 http://earth.geology.yale.edu/~brandon/Eprints/Soloviev_etal1998.pdf |