The Origin of Paleozoic Terranes in Northeastern Asia: Geologic Evidence for Rifting of the Pericratonic Margin of the Siberian Paleocontinent and for Migration of Its Fragments

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The Origin of Paleozoic Terranes in Northeastern Asia: Geologic Evidence for Rifting of the Pericratonic Margin of the Siberian Paleocontinent and for Migration of Its Fragments. / Kanygin, A.; Gonta, T.; Timokhin, A.

в: Russian Geology and Geophysics, Том 61, № 11, 11.2020, стр. 1197-1211.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

BibTeX

@article{1798a5f451a242269fff1ae467a2e159,

title = "The Origin of Paleozoic Terranes in Northeastern Asia: Geologic Evidence for Rifting of the Pericratonic Margin of the Siberian Paleocontinent and for Migration of Its Fragments",

abstract = "The paper provides an insight into the geodynamic history of the Northeast Asian terranes during the Paleozoic, focused on the stratigraphic, paleontological, and sedimentological data indicating that the Precambrian structures of early-middle Paleozoic age were originally part of the passive margin of the Siberian paleocontinent. The geological and paleontological data presented in the foregoing studies have shown the inherited geodynamic regime and synchronous sedimentation and magmatism on the passive continental margin and in most terranes before their separation from the Siberian paleocontinent in the late Paleozoic. The revealed significant differences in evolution between the Okhotsk and Omolon and other terranes give grounds to postulate that they rifted off the paleocontinent even earlier.",

keywords = "orogenic belt, terranes, Paleozoic, tectonics, geodynamics, sedimentology, paleogeography, stratigraphy, northeastern Asia, Siberian paleocontinent, WESTERN BOUNDARY, NORTH-AMERICAN, PALEOMAGNETISM, EVOLUTION, PLATFORM, CONSTRAINTS, TECTONICS, POSITION, HISTORY, RODINIA",

author = "A. Kanygin and T. Gonta and A. Timokhin",

note = "Funding Information: The authors express their most sincere gratitude to N.L. Dobretsov, D.V. Grazhdankin, and D.V. Metelkin for their valuable comments and recommendations, which were extremely important for finalizing the paper. The work was carried out under the International Geological Correlation Programme project No. 653b “The Onset of the Great Ordovician Biodiversity Event” and financially supported by the Russian Foundation for Basic Research grant No. 18-05-00248. Publisher Copyright: {\textcopyright} 2020, V.S. Sobolev IGM, Siberian Branch of the RAS 2020.",

year = "2020",

month = nov,

doi = "10.15372/RGG2019140",

language = "English",

volume = "61",

pages = "1197--1211",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "11",

}

RIS

TY - JOUR

T1 - The Origin of Paleozoic Terranes in Northeastern Asia: Geologic Evidence for Rifting of the Pericratonic Margin of the Siberian Paleocontinent and for Migration of Its Fragments

AU - Kanygin, A.

AU - Gonta, T.

AU - Timokhin, A.

N1 - Funding Information: The authors express their most sincere gratitude to N.L. Dobretsov, D.V. Grazhdankin, and D.V. Metelkin for their valuable comments and recommendations, which were extremely important for finalizing the paper. The work was carried out under the International Geological Correlation Programme project No. 653b “The Onset of the Great Ordovician Biodiversity Event” and financially supported by the Russian Foundation for Basic Research grant No. 18-05-00248. Publisher Copyright: © 2020, V.S. Sobolev IGM, Siberian Branch of the RAS 2020.

PY - 2020/11

Y1 - 2020/11

N2 - The paper provides an insight into the geodynamic history of the Northeast Asian terranes during the Paleozoic, focused on the stratigraphic, paleontological, and sedimentological data indicating that the Precambrian structures of early-middle Paleozoic age were originally part of the passive margin of the Siberian paleocontinent. The geological and paleontological data presented in the foregoing studies have shown the inherited geodynamic regime and synchronous sedimentation and magmatism on the passive continental margin and in most terranes before their separation from the Siberian paleocontinent in the late Paleozoic. The revealed significant differences in evolution between the Okhotsk and Omolon and other terranes give grounds to postulate that they rifted off the paleocontinent even earlier.

AB - The paper provides an insight into the geodynamic history of the Northeast Asian terranes during the Paleozoic, focused on the stratigraphic, paleontological, and sedimentological data indicating that the Precambrian structures of early-middle Paleozoic age were originally part of the passive margin of the Siberian paleocontinent. The geological and paleontological data presented in the foregoing studies have shown the inherited geodynamic regime and synchronous sedimentation and magmatism on the passive continental margin and in most terranes before their separation from the Siberian paleocontinent in the late Paleozoic. The revealed significant differences in evolution between the Okhotsk and Omolon and other terranes give grounds to postulate that they rifted off the paleocontinent even earlier.

KW - orogenic belt

KW - terranes

KW - Paleozoic

KW - tectonics

KW - geodynamics

KW - sedimentology

KW - paleogeography

KW - stratigraphy

KW - northeastern Asia

KW - Siberian paleocontinent

KW - WESTERN BOUNDARY

KW - NORTH-AMERICAN

KW - PALEOMAGNETISM

KW - EVOLUTION

KW - PLATFORM

KW - CONSTRAINTS

KW - TECTONICS

KW - POSITION

KW - HISTORY

KW - RODINIA

UR - http://www.scopus.com/inward/record.url?scp=85133719439&partnerID=8YFLogxK

U2 - 10.15372/RGG2019140

DO - 10.15372/RGG2019140

M3 - Article

VL - 61

SP - 1197

EP - 1211

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 11

ER -

ID: 27358454