Research output: Contribution to journal › Article › peer-review
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.
In: Russian Geology and Geophysics, Vol. 61, No. 11, 11.2020, p. 1197-1211.Research output: Contribution to journal › Article › peer-review
}
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