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Record #180549:
- #180549
Main publication details
MARC recordТепловой поток Баренцевоморского-Карского региона
| Title: | Тепловой поток Баренцевоморского-Карского региона |
| Title, transliterated: | Teplovoĭ potok Barent︠s︡evomorskogo-Karskogo regiona / L.A. T︠S︡ybulʹi︠a︡, L.S. Sokolova. |
| Translated title: | Heat flow in the region of the Barents and Kara seas. |
| Author(s): | T︠S︡ybulʹi︠a︡, L. A. Sokolova, L. S. |
| Date: | 2002. |
| Language: | Russian. |
| In: | Geologii︠a︡ i Geofizika. (2002.), Vol. 43(11) (2002) |
| Abstract: | Compiles and discusses map of heat flow that is synthesis of geothermal data from West Arctic shelf collected since 1980s. Strongly uneven heat flow distribution reflects complex geological and geodynamic settings of region. Heat flows are noticeably lower on continent than in ocean. Generally elevated mantle heat flow on Barents and Kara sea shelves is evidence of hot anomalous mantle apparently associated with recent ocean formation. |
| Notes: | Geologii︠a︡ i Geofizika. Vol. 43(11) :1049-1052 (2002). |
| Keywords: | 550.36 -- Terrestrial energetics and thermodynamics. B -- Geology and soil sciences. (*60) -- Arctic Ocean and adjacent waters. (*686) -- Barents Sea. (*685) -- Kara Sea. |
| SPRI record no.: | 180549 |
LDR 01991naa#a2200000#a#4500 001 SPRI-180549 005 20231002112241.0 007 ta 008 231002s2002####xx#ab#|##|###|0||#0|rus#d 035 ## ‡aSPRI-180549 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 100 1# ‡6880-01‡aT︠S︡ybulʹi︠a︡, L. A. 242 10 ‡aHeat flow in the region of the Barents and Kara seas.‡yeng 245 10 ‡6880-02‡aTeplovoĭ potok Barent︠s︡evomorskogo-Karskogo regiona /‡cL.A. T︠S︡ybulʹi︠a︡, L.S. Sokolova. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2002. 300 ## ‡ap. 1049-1052 :‡bill., map (folded) 500 ## ‡aGeologii︠a︡ i Geofizika. Vol. 43(11) :1049-1052 (2002). 520 3# ‡aCompiles and discusses map of heat flow that is synthesis of geothermal data from West Arctic shelf collected since 1980s. Strongly uneven heat flow distribution reflects complex geological and geodynamic settings of region. Heat flows are noticeably lower on continent than in ocean. Generally elevated mantle heat flow on Barents and Kara sea shelves is evidence of hot anomalous mantle apparently associated with recent ocean formation. 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 ‡a550.36 -- Terrestrial energetics and thermodynamics.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 651 #7 ‡a(*685) -- Kara Sea.‡2udc 700 1# ‡6880-03‡aSokolova, L. S. 773 0# ‡6880-04‡7nnas ‡tGeologii︠a︡ i Geofizika. ‡gVol. 43(11) (2002) ‡wSPRI-35274 880 1# ‡6100-01/(N‡aЦыбулья, Л. А. 880 10 ‡6245-02/(N‡aТепловой поток Баренцевоморского-Карского региона /‡cЛ.А. Цыбулья, Л.С. Соколова. 880 1# ‡6700-03/(N‡aСоколова, Л. С. 880 0# ‡6773-04/(N‡7nnas ‡tГеология и Геофизика. ‡gVol. 43(11) (2002) ‡wSPRI-35274 916 ## ‡a2007/11/14 -- IW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231002 ‡bIW