SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #184100:
Многолетняя динамика толщ мерзлых пород и зоны стабильности гидратов газов в рифтовых структурах Арктического шельфа Восточной Сибири: сообщение 1 / Н.Н. Романовский, А.А. Елисеева, А.В. Гаврилов, Г.С. Тишенко, H.-W Хубертен.
Title: | Многолетняя динамика толщ мерзлых пород и зоны стабильности гидратов газов в рифтовых структурах Арктического шельфа Восточной Сибири: сообщение 1 / Н.Н. Романовский, А.А. Елисеева, А.В. Гаврилов, Г.С. Тишенко, H.-W Хубертен. |
Title, transliterated: | Mnogoletni︠a︡i︠a︡ dinamika tolshch merzlykh porod i zony stabilʹnosti gidratov gazov v riftovykh strukturakh Arkticheskogo shelʹfa Vostochnoĭ Sibiri: soobshchenie 1 / N.N. Romanovskiĭ, A.A. Eliseeva, A.V. Gavrilov, G.S. Tishenko, H.-W Khuberten. |
Translated title: | Long-term dynamics of the permafrost layer and gas hydrate stability zones on rifts of Arctic Shelf of East Siberia: report 1. |
Author(s): | Romanovskiĭ, N. N. Eliseeva, A. A. Gavrilov, A. V. Tishenko, G. S. Hubberten, H. -W. |
Date: | 2005. |
Language: | Russian. |
In: | Kriosfera Zemli. (2005.), Vol. 9(4) (2005) |
Abstract: | Creates tectonic model of rift system of Laptev Sea and compiles palaeogeographic scenarios for last 400 000 years, based on analysis of environmental conditions of East-Siberian Arctic. Mathematical modelling shows that, in course of evolution of permafrost, its thickness above fault zones can be sharply reduced. As result, traps of underground gases and hydrates can develop, as well as open submarine taliks. Studies enable forecasting of formation and evolution of traps and open taliks in rift system of Laptev Sea in connection with geothermal heterogeneity and periodic draining and flooding of shelf. |
Notes: | Kriosfera Zemli. Vol. 9(4) :42-53 (2005). |
Keywords: | 551.8 -- Palaeogeography. 551.34 -- Geocryology. Frozen ground. 551.345 -- Permafrost. Cryopedology. 548.736.65 -- Clathrate hydrates. 551.24 -- Geotectonics. 519.673 -- Modelling. E7 -- Glaciology: glacial geology and ice ages. (*60) -- Arctic Ocean and adjacent waters. (*684) -- Laptev Sea. |
SPRI record no.: | 184100 |
LDR 02879naa#a2200000#a#4500 001 SPRI-184100 005 20240418190053.0 007 ta 008 240418s2005####xx####|##|###|0||#0|rus#d 035 ## ‡aSPRI-184100 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡arus 242 00 ‡aLong-term dynamics of the permafrost layer and gas hydrate stability zones on rifts of Arctic Shelf of East Siberia :‡breport 1.‡yeng 245 00 ‡6880-01‡aMnogoletni︠a︡i︠a︡ dinamika tolshch merzlykh porod i zony stabilʹnosti gidratov gazov v riftovykh strukturakh Arkticheskogo shelʹfa Vostochnoĭ Sibiri :‡bsoobshchenie 1 /‡cN.N. Romanovskiĭ, A.A. Eliseeva, A.V. Gavrilov, G.S. Tishenko, H.-W Khuberten. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2005. 300 ## ‡ap. 42-53. 500 ## ‡aKriosfera Zemli. Vol. 9(4) :42-53 (2005). 520 3# ‡aCreates tectonic model of rift system of Laptev Sea and compiles palaeogeographic scenarios for last 400 000 years, based on analysis of environmental conditions of East-Siberian Arctic. Mathematical modelling shows that, in course of evolution of permafrost, its thickness above fault zones can be sharply reduced. As result, traps of underground gases and hydrates can develop, as well as open submarine taliks. Studies enable forecasting of formation and evolution of traps and open taliks in rift system of Laptev Sea in connection with geothermal heterogeneity and periodic draining and flooding of shelf. 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 ‡a551.8 -- Palaeogeography.‡2udc 650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc 650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc 650 07 ‡a548.736.65 -- Clathrate hydrates.‡2udc 650 07 ‡a551.24 -- Geotectonics.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*684) -- Laptev Sea.‡2udc 700 1# ‡6880-02‡aRomanovskiĭ, N. N. 700 1# ‡6880-03‡aEliseeva, A. A. 700 1# ‡6880-04‡aGavrilov, A. V. 700 1# ‡6880-05‡aTishenko, G. S. 700 1# ‡6880-06‡aHubberten, H. -W. 773 0# ‡6880-07‡7nnas ‡tKriosfera Zemli. ‡gVol. 9(4) (2005) ‡wSPRI-145770 880 00 ‡6245-01/(N‡aМноголетняя динамика толщ мерзлых пород и зоны стабильности гидратов газов в рифтовых структурах Арктического шельфа Восточной Сибири :‡bсообщение 1 /‡cН.Н. Романовский, А.А. Елисеева, А.В. Гаврилов, Г.С. Тишенко, H.-W Хубертен. 880 1# ‡6700-02/(N‡aРомановский, Н. Н. 880 1# ‡6700-03/(N‡aЕлисеева, А. А. 880 1# ‡6700-04/(N‡aГаврилов, А. В. 880 1# ‡6700-05/(N‡aТишенко, Г. С. 880 1# ‡6700-06/(N‡aHуббертен, H. -W. 880 0# ‡6773-07/(N‡7nnas ‡tКриосфера Земли. ‡gVol. 9(4) (2005) ‡wSPRI-145770 916 ## ‡a2008/08/29 -- IW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418 ‡bIW