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Аbstract

South Anyui suture stretches from the east part of the Laptev Sea to western Chukotka. This suture is everywhere marked by Mesozoic terrigenous sequences with ophiolite fragments of Paleozoic and/or Mesozoic age. South of the suture, suprasubduction complexes of Late Paleozoic, Late Triassic, and Late Jurassic to Early Cretaceous age have been reported. Within the suture, besides ophiolites, one finds island arc rocks, deformed turbidites of Late Triassic and Late Jurassic to Early Cretaceous age, and accretionary type terrigenous melange. Accretionary melange and closely coeval suprasubduction complexes are interpreted to point to ancient convergent boundaries between plates of the Proto-Arctic oceanic basin and North Asian continent.