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Record #180541:

Охотское океаническое вулканическое плато

Title: Охотское океаническое вулканическое плато
Title, transliterated: Okhotskoe okeanicheskoe vulkanicheskoe plato / N.A. Bogdanov, N.L. Dobret︠s︡ov.
Translated title: The Okhotsk oceanic volcanic plateau.
Author(s): Bogdanov, N. A.
Dobret︠s︡ov, N. L.
Date: 2002.
Language: Russian.
In: Geologii︠a︡ i Geofizika. (2002.), Vol. 43(2) (2002)
Abstract: Interprets Okhotsk Sea plate as old volcanic oceanic plateau bounded by right-lateral strike-slip faults in east and west, Middle Cretaceous subduction zone in north, and by zone of ongoing subduction of Pacific Plate beneath Eurasia in south. Analysis of internal structure of Okhotsk plate leads to identification of remnant Middle Jurassic-Lower Cretaceous crust on plate margins in accretionary prisms. Concludes that South Okhotsk deepest oceanic basin, south of plate, is most likely of oceanic origin and is largest fragment of Late Cretaceous Kula oceanic plate.
Notes:

Geologii︠a︡ i Geofizika. Vol. 43(2) :101-114 (2002).

Keywords: 551.1/.4 -- Geology.
551.24 -- Geotectonics.
551.241 -- Plate tectonics.
B -- Geology and soil sciences.
(*666) -- Sea of Okhotsk.
SPRI record no.: 180541

MARCXML

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001 SPRI-180541
005 20240328185414.0
007 ta
008 240328s2002####xx#ab#|##|###|0||#0|rus#d
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040 ## ‡aUkCU-P‡beng‡eaacr
041 0# ‡arus
100 1# ‡6880-01‡aBogdanov, N. A.
242 14 ‡aThe Okhotsk oceanic volcanic plateau.‡yeng
245 10 ‡6880-02‡aOkhotskoe okeanicheskoe vulkanicheskoe plato /‡cN.A. Bogdanov, N.L. Dobret︠s︡ov.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2002.
300 ## ‡ap. 101-114 :‡bill., diags., maps.
500 ## ‡aGeologii︠a︡ i Geofizika. Vol. 43(2) :101-114 (2002).
520 3# ‡aInterprets Okhotsk Sea plate as old volcanic oceanic plateau bounded by right-lateral strike-slip faults in east and west, Middle Cretaceous subduction zone in north, and by zone of ongoing subduction of Pacific Plate beneath Eurasia in south. Analysis of internal structure of Okhotsk plate leads to identification of remnant Middle Jurassic-Lower Cretaceous crust on plate margins in accretionary prisms. Concludes that South Okhotsk deepest oceanic basin, south of plate, is most likely of oceanic origin and is largest fragment of Late Cretaceous Kula oceanic plate.
546 ## ‡aIn Russian.
546 ## ‡aRussian transliteration entered into original records using BGN/PCGN 1947 romanisation of Russian; Cyrillic text in MARC 880 field(s) reverse transliterated from this by automated process; BGN/PCGN 1947 text then upgraded to Library of Congress romanisation.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.24 -- Geotectonics.‡2udc
650 07 ‡a551.241 -- Plate tectonics.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*666) -- Sea of Okhotsk.‡2udc
700 1# ‡6880-03‡aDobret︠s︡ov, N. L.
773 0# ‡6880-04‡7nnas ‡tGeologii︠a︡ i Geofizika. ‡gVol. 43(2) (2002) ‡wSPRI-35274
880 1# ‡6100-01/(N‡aБогданов, Н. А.
880 10 ‡6245-02/(N‡aОхотское океаническое вулканическое плато /‡cН.А. Богданов, Н.Л. Добрецов.
880 1# ‡6700-03/(N‡aДобрецов, Н. Л.
880 0# ‡6773-04/(N‡7nnas ‡tГеология и Геофизика. ‡gVol. 43(2) (2002) ‡wSPRI-35274
916 ## ‡a2007/11/14 -- IW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328 ‡bIW