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СПИСЪК на цитиранията на. д-р Атанас Димитров Василев след ...

СПИСЪК на цитиранията на. д-р Атанас Димитров Василев след ...

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<strong>СПИСЪК</strong><strong>на</strong> <strong>цити<strong>р</strong>анията</strong> <strong>на</strong>. <strong>д</strong>-<strong>р</strong> Ата<strong>на</strong>с Димит<strong>р</strong>ов <strong>Василев</strong> сле<strong>д</strong> п<strong>р</strong>и<strong>д</strong>обиване <strong>на</strong>ака<strong>д</strong>емич<strong>на</strong> <strong>д</strong>лъжност “<strong>д</strong>оцент”Nota Bene:1. П<strong>р</strong>е<strong>д</strong>ставени са 75 цити<strong>р</strong>ания, 55 от които са отбелязани като по-важни су<strong>д</strong>ебелен ш<strong>р</strong>ифт (<strong>на</strong>п<strong>р</strong>име<strong>р</strong> в списания с Импакт факто<strong>р</strong>);2. Някои от цити<strong>р</strong>аните публикации са от списъка <strong>д</strong>о п<strong>р</strong>и<strong>д</strong>обиване <strong>на</strong>ака<strong>д</strong>емич<strong>на</strong> <strong>д</strong>лъжност “<strong>д</strong>оцент”, но цитатите са публикувани сле<strong>д</strong> по<strong>д</strong>аване <strong>на</strong><strong>д</strong>окументите за “<strong>д</strong>оцент” (2003);3. Този списък не е пълен - не е п<strong>р</strong>авено специално тъ<strong>р</strong>сене за цити<strong>р</strong>ания.4. П<strong>р</strong>име<strong>р</strong>ните тъ<strong>р</strong>сения с google.com са неточни, но показват какъв п<strong>р</strong>облем етъ<strong>р</strong>сенето, когато отсъства або<strong>на</strong>мент за п<strong>р</strong>офесио<strong>на</strong>лните Инте<strong>р</strong>нет с<strong>р</strong>е<strong>д</strong>ства.5. Пълните публикации с цити<strong>р</strong>ания са <strong>на</strong> п<strong>р</strong>иложения CD/DVD: folder“Citations”. Име<strong>на</strong>та <strong>на</strong> файловете започват с „С” за „Citations” и номе<strong>р</strong>,съответстващ <strong>на</strong> номе<strong>р</strong>а <strong>на</strong> цити<strong>р</strong>ане от списъка, а п<strong>р</strong>иложените г<strong>р</strong>афичниилюст<strong>р</strong>ации са PNG файлове с име<strong>на</strong> като “C4-1.PNG”.Кутас Р. И., В. П. Коболев, В. А. Цвященко, А. Д. Васильев, О. П. К<strong>р</strong>авчук, 1992. Новыеоп<strong>р</strong>е<strong>д</strong>еления тепловых потоков в болга<strong>р</strong>ском секто<strong>р</strong>е Че<strong>р</strong>ного мо<strong>р</strong>я. Докла<strong>д</strong>ыАка<strong>д</strong>емии <strong>на</strong>ук Ук<strong>р</strong>аины, 7, 104-107.Цитат в:1. Poort J., A. Vassilev, L. Dimitrov, 2005. Did postglacial catastrophic floodingtrigger massive changes in the Black Sea gas hydrate reservoir? Terra Nova,17 (2), 135–140.Vassilev A., 1994. Bulgarian Black Sea region – the deepwater oil and gas potential of theCenozoic sequence.. International Symposium: Petroleum geology and hydrocarbon potentialof the Black Sea area, P-24, 16-18 October 1994, Varna, Bulgaria.Цитат в:2. Димит<strong>р</strong>ов Л., 2003. Плитко залягащи газо<strong>на</strong>ситени утайки и газоп<strong>р</strong>оявления<strong>на</strong> бълга<strong>р</strong>ския континентален шелф. Авто<strong>р</strong>ефе<strong>р</strong>ат)Vassilev A., 1996. Oil and gas potential of the Bulgarian Black Sea part (the PaleogeneSequence). In: Petroleum Potential of the Balkan Region, Sofia, 327-342.Цитат в:3. Димит<strong>р</strong>ов Л., 2003. Плитко залягащи газо<strong>на</strong>ситени утайки и газоп<strong>р</strong>оявления<strong>на</strong> бълга<strong>р</strong>ския континентален шелф. Авто<strong>р</strong>ефе<strong>р</strong>атVassilev, A., L. Dimitrov, 2000. Spatial and quantity evaluation of methane hydrates in theBlack Sea. Proceedings of the 6th Conference "Gas in Marine Sediments", St. Petersburg,Russia.Цитат в:4. Popescu I., G. Lericolais, N. Panin, A. Normand, C. Dinu, E. Le Drezen,2004. The Danube submarine canyon (Black Sea): morphology andsedimentary processes. Marine Geology, 206, 249-265.Vassilev, A., 2000. Contribution to Atmosphere Hydrocarbons from Black SeaThermogenetic Gases during the Basin Evolution, Third National Geophysical Conference,Sofia, pp. 57-59.


Цитат в:5. http://www.ifremer.fr/assemblage/d6a-reference_list.htmVassilev, A., L. Dimitrov, 2002. Spatial and qualitative evaluation of the Black Sea gashydrates (in Russian and English). Russian Geology and Geophysics, Vol. 43, No. 7, 637-649.Цитат в:6. Tender Documents Prospecting and exploration permit for oil and gas inBlock “Varna – Deep Sea” (Конку<strong>р</strong>сни Документи Раз<strong>р</strong>ешение за тъ<strong>р</strong>сенеи п<strong>р</strong>оучване <strong>на</strong> нефт и газ в блок “Ва<strong>р</strong><strong>на</strong> – <strong>д</strong>ълбоко мо<strong>р</strong>е”), Ministry ofEnvironment and Waters, Sofia, June, 2002).7. http://www.gashydat.org8. Ludmann T., H. K. Wong, P. Konerding, M. Zillmer, J. Petersen, E. Fluh,2004. Heat flow and quantity of methane deduced from a gas hydrate field inthe vicinity of the Dnieper Canyon, northwestern Black Sea. Geo-MarineLetters 24, 182–193.9. Shnyukov E. F., A. P. Ziborov, 2004. Mineral resources of the Black Sea (inRussian). NASU, Kiev, 370 p.10. Popescu I., G. Lericolais, N. Panin, A. Normand, C. Dinu, E. Le Drezen,2004. The Danube submarine canyon (Black Sea): morphology andsedimentary processes. Marine Geology, Vol. 206, Is. 1–4, 249-265.• Kruglyakova R., Y. Byakov, M. Kruglyakova, L. Chalenko, N. Shevtsova,2004. Geo-Mar Lett, 2004, 24, 150-16211. Roberts A., Richard Weaver, 2005. Multiple mechanisms of remagnetizationinvolving sedimentary greigite (Fe 3 S 4 ). Earth and Planetary Science Letters,Vol.231, Is. 3–4, 263-277.12. Max M. D., A.H. Johnson,W. P. Dillon, 2006. Economic Geology of NaturalGas Hydrate. Coastal Systems and Continental Margins, Springer, ISBN-101-4020-3971-9 (HB), 341 p.13. http://gasoilpress.com/dgir/dgir_detailed_work.php?DGIR_ELEMENT_ID=283&WORK_ELEMENT_ID=5637 (2006)14. Kessler J. D., W. S. Reeburgh, J. Southon, R. Seifert, W. Michaelis, S. C.Tyler, 2006. Basin-wide estimates of the input of methane from seeps andclathrates to the Black Sea. Earth and Planetary Science Letters, 243, 366–375.15. Popescu I., M. DeBatist, G. Lericolais, H. Nouzé, J. Poort, N. Panin, W.Versteeg, H. Gillet, 2006. Multiple bottom-simulating reflections in the BlackSea, Potential proxies of past climate conditions. Marine Geology,DOI:10.1016/j.margeo.2005.12.006 (3 цитата).16. Schmale, Oliver, 2006. Submarine methane seepage in the paleo Dnepr areaand Sorokin Trough and its influence on the Black Sea methane budget.Dissertation, Christian-Albrechts-Universitat, Kiel (http://e-diss.unikiel.de/diss_1920/d1920.pdf)(8 цитата)17. www.cambridge.org/resources/0521819504/4334_L_L.Dimitrov.ppt18. Bulbul, Sevtak, 2007. Hydrate formation conditions of methane hydrogensulfide mixtures, METU, Thesis, 104 p.19. Popescu I., G. Lericolais, N. Panin, M. DeBatist, H. Gillet, 2007. Seismicexpression of gas and gas hydrates across the western Black Sea. Geo-Marine Letters, DOI: 10.1007/s00367-007-0068-0.20. www.cambridge.org/resources/0521819504/4323_Introduction.ppt (Introductionto Power Point presentations accompanying the book ‘Seabed Fluid Flow’ byAlan Judd and Martin Hovland, 2007)21. Alan Judd & Martin Hovland, 2007. Seabed Fluid Flow (The Impact onGeology, Biology and the Marine Environment). Cambridge University


Press, 492 p. (ISBN-13: 9780521819503 | ISBN-10: 0521819504) DOI:10.2277/052181950422. Schmid M., M. De Batist, N. Granin, V. Kapitanov, D. McGinnis, I.Mizandrontsev, A. Obzhirov, A. Wuest, 2007. Sources and sinks of methanein Lake Baikal: A synthesis of easurements and modeling. Limnol.Oceanogr., 52/5, 1824-1837.23. Schmale, O. et al., 2009. Gas seepage in the Dnepr paleo-delta area (NW-Black Sea) and its regional impact on the water column methane cycle,Journal of Marine Systems, doi:10.1016/j.jmarsys.2009.10.00324. Timothy A. Minshull and Aaron Keddie, 2010. Measuring the geotherm withgas hydrate bottom-simulating reflectors: a novel approach using threedimensionalseismic data from the eastern Black Sea. Terra Nova, 22, 131–13625. Sosson et al. (ed), 2010. Sedimentary basin tectonics from the Black Sea andCaucasus to the Arabian Platform. Ondon. ISBN 9781862393080, GeologicalSociety, no. 340, 509 p.26. Heeschen K., M Haeckel, I Klaucke, M K Ivanov, G Bohrmann, 2011.Quantifying in-situ gas hydrates at active seep sites in the eastern Black Seausing pressure coring technique. Biogeosciences Discuss., 8, 4529-4558.Вассилев А., Л. Димит<strong>р</strong>ов, 2002. Оценка п<strong>р</strong>ост<strong>р</strong>анственного <strong>р</strong>асп<strong>р</strong>е<strong>д</strong>еления и запасовгазоги<strong>д</strong><strong>р</strong>атов в Че<strong>р</strong>ном мо<strong>р</strong>е. Геология и геофизика, Новосиби<strong>р</strong>ск, СО РАН, т. 43, № 7,672-684.Цитат в:27. http://cat.inist.fr/?aModele=afficheN&cpsidt=1460255028. Пе<strong>р</strong>лова Е. В., С. А. Леонов, В. С. Якушев, Н. А. Махони<strong>на</strong>, 2006.Субаквальные газоги<strong>д</strong><strong>р</strong>аты: геология, геохимия, пе<strong>р</strong>спективыосвоения. Газовые ги<strong>д</strong><strong>р</strong>аты (Спецвыпуск: Газовая п<strong>р</strong>омышленност), М,7-11.29. К<strong>р</strong>углякова, Р., М. К<strong>р</strong>углякова, Н. Шевцова, 2009. Геологогеохимическаяха<strong>р</strong>акте<strong>р</strong>истика естественных п<strong>р</strong>оявленийуглево<strong>д</strong>о<strong>р</strong>о<strong>д</strong>ов в Че<strong>р</strong>ном мо<strong>р</strong>е. Геология и полезные ископаемыеМи<strong>р</strong>ового океа<strong>на</strong>, № 1, 37-51.Vassilev, A., 2002.Bulgarian Black Sea Continental Slope -Oil and Gas Potential of theCenozoic Sequence.Цитат в:30. http://www.eastoil.com (http://209.238.195.142/bulgaria/bgrepinv.htm)Vassilev, A., L. Dimitrov, 2003. Bulgarian national program for gas hydrates research.Цитат в:31. http://www.mgu.bg/sessions/03/1/mv_ld.pdf32. http://mgu.bg/annual/public_html/2004/en/svityk1/dokladi_pdf/Vasilev_en.pdf33. http://www.io-bas.bg/cesum-bs/npghen/bsgh.htmVassilev, A., 2003. Black Sea Basin: 65 Million Years Methane Breath. Comptes Rendus del'Academie bulgare des Sciences, Vol. 56, No. 3, 9-14.Цитат в:34. http://adsabs.harvard.edu/full/2003CRABS..56c...9V35. http://cat.inist.fr/?aModele=afficheN&cpsidt=14602549Vassilev, A., L. Dimitrov, 2003. Model evaluation of the Black Sea gas hydrates. ComptesRendus de l'Academie bulgare des Sciences, Vol. 56, No. 3, 15-19.Цитат в:36. http://direct.bl.uk/bld/PlaceOrder.do?UIN=144908776&ETOC=RN&from=searchengine (British Library)37. http://cat.inist.fr/?aModele=afficheN&cpsidt=14602550


38. http://adsabs.harvard.edu/full/2003CRABS..56c..15VVassilev, А., 2003. Quaternary Black Sea Methane Hydrates. EGS - AGU - EUG JointAssembly, Nice, France, 6-11 April 2003 (Extended Abstract).Цитат в:39. http://www.cosis.net/abstracts/EAE03/09721/EAE03-J-09721.pdfDimitrov L., A.Vassilev, 2003. Black Sea gas seepage and venting structures and their contribution toatmospheric methane (in English and Bulgarian). Proceedings of Jubilee InternationalScientific Session 50 years UMG ”St. Ivan Rilski”, 14-16 May 2003 Sofia, Bulgaria.Цитатв:40. http://www.metaftp.com/?t=searchresults&PageId=2&OrderType=-1&ServerId=9075796Poort, J., Kutas, R., Vssilev, A., Klerkx, J. and De Batist, M., 2004. Heat flow variability inthe seep dominated northern margin of the Black Sea, 32nd International GeologicalCongress, Florence, Italy, pp. 1252.Цитат в:41. http://www.ifremer.fr/assemblage/d6a-reference_list.htmVassilev А., 2004. Gas hydrate stability zone model & methane seeps of the north Bulgarianoffshore. ASSEMBLAGE Workshop, 23-26 October 2004, Varna (Extended Abstract & MSPP Presentation).Цитат в:42. http://www.ifremer.fr/assemblage/documents/Varna_Workshop/Varna-17-Vassilev2.pdfVassilev А., 2004. 4D history of the Black Sea basin methane emission (How to predict thefuture climate looking in the past). ASSEMBLAGE Workshop, 23-26 October 2004, Varna(Extended Abstract & MS Power Point Presentation).Цитат в:43. http://www.ifremer.fr/assemblage/documents/Varna_Workshop/Varna-16-Vassilev1.pdfPoort, J., Kutas, R., Vassilev, A., Klerkx, J., 2005. Heat flow variability in the seep dominatednothern margin of the Black Sea. (Abstract), Proceedings of the VIII International ConferenceGas in Marine Sediments, Univeristy of Vigo, Spain, Sept. 5-10, 2005.Цитат в:44. AAPG/GSTT Hedberg Conference “Mobile Shale Basins – Genesis, Evolutionand Hydrocarbon Systems “ June 4-7, 2006 – Port of Spain, Trinidad & TobagoMud volcanoes – a result of supercritical water formation at depth? MartinHovland, Håkon Rueslåtten, Helge Løseth, Christine Fichler, Hans KonradJohnsen.45. Schmale O., S.E. Beaubien, G. Rehder, J. Greinert, S. Lombardi, 2010. Gasseepage in the Dnepr paleo-delta area (NW-Black Sea) and its regionalimpact on the water column methane cycle. Journal of Marine Systems,80,/1–2, 90-100.Poort J., A. Vassilev, L. Dimitrov, 2005. Did postglacial catastrophic flooding trigger massivechanges in the Black Sea gas hydrate reservoir? Terra Nova, 17 (2), 135–140. (И<strong>д</strong>ея, <strong>д</strong>анни,тео<strong>р</strong>ия и алго<strong>р</strong>итми <strong>на</strong> кан<strong>д</strong>и<strong>д</strong>ата; Dr Poort - изчисления и текст по в<strong>р</strong>еме <strong>на</strong>специализацията му в ИО-БАН, Ва<strong>р</strong><strong>на</strong> по п<strong>р</strong>оект CESUM-BS)Цитат в:46. Lieven N., J. Greinert., Y. Artemov., P. Staelens., J. Poort., P. VanRensbergen., Marc De Batist, 2006. Geological and morphological setting of2778 methane seeps in the Dnepr paleo-delta, northwestern Black Sea.Marine Geology, 227. 177– 199.47. Schmale, Oliver, 2006. Submarine methane seepage in the paleo Dnepr areaand Sorokin Trough and its influence on the Black Sea methane budget.


Dissertation, Christian-Albrechts-Universitat, Kiel (http://e-diss.unikiel.de/diss_1920/d1920.pdf)(4 цитата)48. Poort J., R. I. Kutas, J. Klerkx, S. E. Beaubien, S. Lombardi, L. Dimitrov, A.Vassilev, L. Naudts, 2007. Strong heat flow variability in an active shallowgas environment, Dnepr palaeo-delta, Black Sea. Geo-Marine Letters, 27:2-4, 185.49. Bulbul, Sevtak, 2007. Hydrate formation conditions of methane hydrogensulfide mixtures, METU, Thesis, 104 p.50. Schmale, O. et al., 2009. Gas seepage in the Dnepr paleo-delta area (NW-Black Sea) and its regional impact on the water column methane cycle,Journal of Marine Systems, doi:10.1016/j.jmarsys.2009.10.00351. Timothy A. Minshull and Aaron Keddie, 2010. Measuring the geotherm withgas hydrate bottom-simulating reflectors: a novel approach using threedimensionalseismic data from the eastern Black Sea. Terra Nova, 22, 131–13652. http://www.earth-pages.com/submit.asp?ref=0954-487953. http://www.crimea-info.org/project3/public0.htm54. http://direct.bl.uk/bld/PlaceOrder.do?UIN=166728147&ETOC=RN&from=searchengine (British Library)Vassilev Atanas, 2005. Gas Hydrates as Sources of Huge Methane Seepages (Case study:Paleo-Dnepr & Dvurechenskii, Black Sea). Geophysical Research Abstracts, EGU 2005,(Extended Abstract)Цитат в:55. http://meetings.copernicus.org/www.cosis.net/abstracts/EGU05/04613/EGU05-J-04613.pdfVassilev, A., 2006. Optimistic and Pessimistic Model Assessments of the Black Sea GasHydrates. Comptes Rendus de l'Academie bulgare des Sciences, Vol. 59, No. 5, 543-550.Цитат в:56. http://cat.inist.fr/?aModele=afficheN&cpsidt=1791687957. Bahr A., T. Pape, F. Abegg, G. Bohrmann, T. van Weering, M.K. Ivanov,2010. Authigenic carbonates from the eastern Black Sea as an archive forshallow gas hydrate dynamics – Results from the combination of CT imagingwith mineralogical and stable isotope analyses. Marine and PetroleumGeology, 27/9, 1819-1829.58. Schwalenberg K., M. Haeckel, J. Poort, M. Jegen, 2010. Evaluation of gashydrate deposits in an active seep area using marine controlled sourceelectromagnetics: Results from Opouawe Bank, Hikurangi Margin, NewZealand, Marine Geology, 272/1–4, 79-88.59. Dimitrov D., 2010. Geology and Non-traditional resources of the Black Sea:Non-traditional resources from Black sea bottom and their possibilities touse as complex raw material. ISBN-10: 3838386396, LAP LAMBERTAcademic Publishing, 244 p.60. Pape T., A. Bahr, S. Klapp, F. Abegg, G. Bohrmann, 2011. Highintensitygas seepage causes rafting of shallow gas hydrates in thesoutheastern Black Sea. Earth and Planetary Science Letters, Vol. 307,Is. 1-2, 35-46.61. http://www.refdoc.fr/Detailnotice?cpsidt=17916879&traduire=en62. http://direct.bl.uk/bld/PlaceOrder.do?UIN=191650231&ETOC=RN&from=searchengine (British Library)63. http://www.proceedings.bas.bg/2006_5_cntent.html#


Vasilev Atanas, Emil Botev, Raina Hristova, 2006. Dvurechenskii Mud Volcano – age andtemporal variable activity from earthquakes, tsunamis and geological samples. NationalConference “Geosciences 2006”, Sofia 31 Nov – 1 Dec 2006(Extended Abstract; MS PowerPoint Presentation – 16.902 MB)Цитат в:64. http://www.bgd.bg/CONFERENCES/Geonauki_2006/Sbornik/pfd_files/60.pdfVasilev Atanas, Emanuil Kojuharov, Jean-Paul Foucher, Gilles Lericolais, Jeffrey Poort, JeanKlerkx, Mark De Batist,2006. Shared optimistic-pessimistic model of the Black Sea gashydrates. National Conference “Geosciences 2006”, Sofia 31 Nov – 1 Dec 2006 (ExtendedAbstract; Poster A0 format)Цитат в:65. http://www.bgd.bg/CONFERENCES/Geonauki_2006/Sbornik/pfd_files/61.pdfVassilev A., Botev E., Hristova R.,2006. Dvurechenskii Mud Volcano, Black Sea: Long TermActivity from Sedimentation, Seismicity and Tsunami Data. Comptes Rendus de l'Academiebulgare des Sciences, Vol. 59, No. 11, 1181-1186.Цитат в:66. Etiope, G., 2009. Natural emissions of methane from geological seepage inEurope. Atmospheric Environment, Vol. 43, Is. 7, 1430-1443.67. http://direct.bl.uk/bld/PlaceOrder.do?UIN=205215826&ETOC=RN&from=searchengine (British Library)68. http://www.proceedings.bas.bg/cgi-bin/mitko/0DOC_abs.pl?2006_b_1369. http://cat.inist.fr/?aModele=afficheN&cpsidt=1850822570. Бог<strong>д</strong>анов М. (<strong>р</strong>е<strong>д</strong>.) Гео Риск, 2010, И-т физики Земли РАН, Москва, 64ст<strong>р</strong>. (http://www.geomark.ru/upload/GR_2010_3.pdf)Poort J., R. I. Kutas, J. Klerkx, S. E. Beaubien, S. Lombardi, L. Dimitrov, A. Vassilev, L.Naudts, 2007. Strong heat flow variability in an active shallow gas environment, Dneprpalaeo-delta, Black Sea. Geo-Marine Letters, 27:2-4, 185-195. DOI 10.1007/s00367-007-0072-4.Цитат в:71. Naudts L., J. Greinert, J. Poort, J. Belza, E. Vangampelaere, D. Boone, P.Linke, J.-P. Henriet, M. De Batist, 2010. Active venting sites on the gashydrate-bearingHikurangi Margin, off New Zealand: Diffusive- versusbubble-released methane, Marine Geology, 272/1–4, 233-250.Vasilev, Atanas, 2010. First Bulgarian Gas Hydrates: Assessment from Probable BSRs.Geology and Mineral Resources of the World Ocean (Геология и полезные ископаемыеМи<strong>р</strong>ового океа<strong>на</strong>), ISSN 1999-7566, National Academy of Sciences of Ukraina, Kiev, No.2, 22-26. (in English)Цитат в:72. http://www.nbuv.gov.ua/portal/natural/gpimo/2010_2/Vasilev.pdf73. http://elibrary.ru/item.asp?id=15122640Vasilev, A., 2010. Bulgarian gas hydrates and bottom instability, AAPG European RegionalAnnual Conf. “Exploration in the Black Sea and Caspian Regions”, Kiev, Ukraine, 17-19 Oct.2010 (Extended Abstract)Цитат в:74. http://www.searchanddiscovery.com/abstracts/pdf/2010/kiev/abstracts/ndx_Vassilev.pdf


Vasilev, A., 2010. Bulgarian gas hydrates: assessment from PBSR, AAPG European RegionalAnnual Conf. “Exploration in the Black Sea and Caspian Regions” , Kiev, Ukraine, 17-19Oct. 2010 (Extended Abstract)Цитат в:75. http://www.searchanddiscovery.com/abstracts/pdf/2010/kiev/abstracts/ndx_Vassilev02.pdfVasilev, A., 2010. Bulgarian gas hydrates: assessment from PBSR, 10th InternationalConference on Gas in Marine Sediments, Listvyanka, Russia, 6-12 September, 2010(Extended Abstract, 2 Fig.)Цитат в:76. http://lin.irk.ru/pdf/10001.pdfСтатистика от тъ<strong>р</strong>сене в Google (неп<strong>р</strong>е<strong>д</strong>ставител<strong>на</strong>, но показател<strong>на</strong>):16,500 ст<strong>р</strong>аници vassilev "black sea"645,000 "vassilev" hydrates14,000 vassilev "heat flow"1,480 vassilev "institute of oceanology"

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