PHANEROZOIC TECTONIC EVOLUTION OF THE CIRCUM-NORTH PACIFIC

dc.contributor.authorNokleberg W.J.
dc.contributor.authorScholl D.W.
dc.contributor.authorParfenov L.M.
dc.contributor.authorMonger J.W.H.
dc.contributor.authorNorton I.O.
dc.contributor.authorKhanchuk A.I.
dc.contributor.authorStone D.B.
dc.contributor.authorScotese C.R.
dc.contributor.authorFujita K.
dc.date.accessioned2021-02-14T10:37:00Z
dc.date.available2021-02-14T10:37:00Z
dc.date.issued2001
dc.description.abstract2000.08 Phanerozoic tectonic evolution of the Circum-North Pacific Author: Nokleberg, Warren J; Parfenov, Leonid M; Monger, James W H; Norton, Ian O; Khanchuk, Alexander I; Stone, David B; Scotese, Christopher R; Scholl, David W; Fujita, Kazuya Abstract: The Phanerozoic tectonic evolution of the Circum-North Pacific is recorded mainly in the orogenic collages of the mountain belts that separate the North Pacific from the eastern North Asian and western North American cratons. The geologic history of the terranes and overlap assemblages that constitute these orogenic collages is highly complex because of post-accretion dismemberment and translation during strike-slip faulting that occurred subparallel to the continental margins.
dc.identifierhttps://elibrary.ru/item.asp?id=13361655
dc.identifier.citationGeological Survey Professional Paper (United States), 2001, , 1626, 1-102
dc.identifier.issn1044-9612
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/24915
dc.titlePHANEROZOIC TECTONIC EVOLUTION OF THE CIRCUM-NORTH PACIFIC
dc.typeСтатья

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