Department of the Interior Us Geological Survey

Total Page:16

File Type:pdf, Size:1020Kb

Department of the Interior Us Geological Survey DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY WEST SIBERIAN OIL-GAS PROVINCE by Peterson, James A. and o Clarke, James W. Open-File Report 89-192 This report is preliminary and has not been re" "owed for conformity with U.S. Geological Survey editorial standards. Any use of trade, product, or firm nair.es is for descriptive purposes only and does not imply endorsement by the U.S. Government. .Missoula, Montana '- 2Reston, VA Table of Contents Introduction......................................................... 1 Structure ......................................................... 3 Introduction................................................... 3 Basement....................................................... 4 Triassic rifts................................................. 8 Mesozoic-Cenozoic cover....................................... 11 Discussion.................................................... 15 Stratigraphy and Paleogeography..................................... 17 Introduction.................................................. 17 Basement...................................................... 17 Unmetamorphosed Paleozoic Rocks of Intermediate Complex........................... 17 Mesozoic-Cenozoic Sedimentary rocks........................... 29 Triassic................................................ 36 Lower and Middle Jurassic............................... 38 Upper Jurassic.......................................... 43 Cretaceous-Neocomian.................................... 47 Cretaceous-Aptian, Albian, and Cenomanian............... 57 Upper Cenozoic.......................................... 76 Petroleum Geology Introduction.................................................. 79 Intermediate Stage............................................ 93 Platformal Triassic........................................... 97 Jurassic...................................................... 98 Neocomian.................................................... 105 Aptian-Albian-Cenomanian..................................... 118 Conclusion ....................................................... 122 Acknowledgements................................................... 124 Selected References................................................ 125 List of Illustrations Page Figure 1. Location of We*t Siberian oil-gas province. .................. 2 Figure 2. Structure of pre-Jurassic basement of West Siberia. .......... 5 Figure 3. Rift systems of basement. .................................... 9 Figure 4. Profile of Koltogor-Urengoy graben. ......................... 10 Figure 5. Structure contours on the Upper Jurassic Bazhenov Formation. .................................................. 12 Figure 6. Structure contours on lower Aptian reflecting horizon. ...... 13 Figure 7. Super-order and first-order structures of West Siberian platform. ................................................... 14 Figure 8. Geographic map of West Siberia, showing political regions, main river systems, mountain ranges, and areas of fossil and Holocene permafros t. .................................... 18 Figure 9. Mesozoic paleogeographic map of West Siberian basin and adj acent arectS. ............................................. 19 Figure 10. Stratigraphic section of West Siberian oil-gas province. .... 20 Figure lOa. Geologic sections of West-Siberian oil-gas province. ........ 21 Figure lOb. Location map of sections showin in fig. lOa. ................ 23 Figure 11. Main basins of pre-Jurassic, West Siberian basin. ......... 24 Figure 12. Isopach map, pre-Jurassic Intermediate Complex. ............. 25 Figure 13. Generalized distribution of middle Paleozoic rocks ir. Intermediate Complex of West Siberian basin. ................ 26 Figure 14. Generalized, distribution of upper Paleozoic rocks in Intermediate Complex of West Siberian basin. .................. 27 Figure 15. Thickness of post-Paleozoic sedimentary cover, West Siberian basin. ............................................. 30 Figure 16. Thickness of post-Triassic sedineni.ary cover. Cross- section lines of figures 17-19 are shown. ................... 31 Figure 17. North-south structural-stratigraphic facies cross-section A-A'-A", South Kara Sea to south border of West Siberian basin.Sea level datum. ................. .............. 33-33a 11 Figure 18. West-east structural-stratigraphic facies cross-section B-B', near-Ural region across Middle Ob region tc eastern border of West Siberian basin. ............................ 34 Figure 19. Wesc-east structural-stratigraphic facies cross-section C-C', near-Ural regior; across Urengoy uplift area to northeast border of basin. ................................ 35 Figure 20. Thickness and general sedimentary facies, Triassic System. .. 37 Figure 21. Thickness, general sedimentary facies and oil and gas fields, Early and Middle Jurassic. ........................ 39 Figure 22. Paleogeographic-sedimentary environment map, Aalenian (Middle Jurassic). ........................................ 40 Figure 23. Paleogeographic-sedimentary environment map, Bajocian- Bathonian (Middle Jurassic). ............................... 41 Figure 24. Paleogeographic-sedimentary environment map, Callovian (Middle Jurassic). ........................................ 42 Figure 25. Thickness, general sedimentary facies, and oil and gas fields, Late Jurassic. ..................................... 44 Figure 26. Paleogeographic-sedimentary environment map, Oxfordian- Fimmerid~ian (Late Jurassic). ............................. 45 Figure 27. Paleogeographic-sedimentary environment map, Volgian (Late Jurassic). .......................................... 46 Figure 28. Thickness, general sedimentary facies, and oil and gas fields, Volgian (Late Jurassic) and lower Beiriasian (Early Cretaceous). .......................................... ... 48 Figure 29. Thickness and general sedimentary facies, Neocc,..ian (Earl} Cretaceous). .............................................. 49 Figure 30. Thickness, general sedimentary facies, and oil and gas fields, upper Berriasian-Lower Valanginian. ............... 50 Figure 31. Thickness, general sedimentary facies. and oil and gas" fields, upper Valanginian (Early Cretaceous). ............... 51 Figure 32. Paleogeographic-sedimentary environment map, Valanginian (Early Cretaceous). ....................................... 52 Figure 33. Thickness, general sedimentary facies, and oil and gas fields, lower Hauterivian (Early Cretaceous). ............. 53 Figure 34. Thickness, general sedimentary facies and oil and gas fields, upper Hauterivian-Barremian (Early Cretaceous). ... 54 111 Figure 35. Paleogeographic-sedimentary environment map, Kauterivian (Early Cretaceous). ....................................... 55 Figure 36, Paleogeographic-sedimentary environment map, Barremian (Early Cretaceous). ................................... ... 56 Figure 37. Thickr-is, general sedimentary fades, and oil end gas fields, Aptian (Early Cretaceous). .......................... 58 Figure 38. Paleogeographic-sedimentary environment map, Aptian (Early Cretaceous). ....................................... 59 Figure 39. Thickness, general sedimentary facies, and oil and gas fields, upper Albian-Cenomanian (Early and Late Cretaceous)................................................. 60 Figure 40. Paleogeographic-sedimentary environment map, Albian (Early Cretaceous). ........................................ 61 Figure 41. Paleogeographic-sedimentary environment map, Cenomanian (Late Cretaceous). ......................................... 62 Figure 42. Thickness and general sedimentary facies, Late Cretaceous without Cenomanian. ....................................... 64 Figure 43. Paleogeographic-sedimentary environment map, Turonian (Late Cretaceous). ........................................ 65 Figure 44. Paleogeographic-sedimentary c 'ironment map, Coniacian (Late Cretaceous). ........................................ 65 Figure 45. Paleographic-sedimentary environment map, Santonian (Late Cretaceous). .............................................. 67 Figure 46. Paleogeographic-sedimentary environment map, Campanian (Late Cretaceous). ........................................ 68 Figure 47. Paleogeographic-sedimentary environment mcp, Maastrichtian (Late Cretaceous). ........................................ 69 Figure 48. Paleogeographic-sedimentary environment map, Danian (Late Oreticeous-early Tertiary?). .............................. 70 Figure 49. Thickness and general sedimentary facies, Tertiary: Paleocene, Eocene, and early Oligocene. ................... 71 Figure 50. Paleogeographic-sedimentary environment map, Paleocene (early Tertiary). ......................................... 72 Figure 51. Paleogeographic-sediir.?ntary environment map, early and middle Eocene (early Tertiary). ............................ 73 IV Figure 52. Paleogeographic-sedimentary environment map, late Eocene (early Tertiary) ......................................... 74 Figure 53. Paleogeographic-sedimentary environment map, Oligocene (early Tertiary). .......................................... 75 Figure 54. Thickness and general sedimentary facies, late Tertiary, Neogene without late Pliocene. ............................ 77 Figure 55. Paleogeographic-sedimentary environment map, early and middle Miocene (late Tertiary). ........................... 78 Figure 56. Petroleum regions, West Siberian basin. ..................... 80 Figure 57. Oil and gas field map, showing main oil and gps fields, West Siberian
Recommended publications
  • FSC National Risk Assessment
    FSC National Risk Assessment for the Russian Federation DEVELOPED ACCORDING TO PROCEDURE FSC-PRO-60-002 V3-0 Version V1-0 Code FSC-NRA-RU National approval National decision body: Coordination Council, Association NRG Date: 04 June 2018 International approval FSC International Center, Performance and Standards Unit Date: 11 December 2018 International contact Name: Tatiana Diukova E-mail address: [email protected] Period of validity Date of approval: 11 December 2018 Valid until: (date of approval + 5 years) Body responsible for NRA FSC Russia, [email protected], [email protected] maintenance FSC-NRA-RU V1-0 NATIONAL RISK ASSESSMENT FOR THE RUSSIAN FEDERATION 2018 – 1 of 78 – Contents Risk designations in finalized risk assessments for the Russian Federation ................................................. 3 1 Background information ........................................................................................................... 4 2 List of experts involved in risk assessment and their contact details ........................................ 6 3 National risk assessment maintenance .................................................................................... 7 4 Complaints and disputes regarding the approved National Risk Assessment ........................... 7 5 List of key stakeholders for consultation ................................................................................... 8 6 List of abbreviations and Russian transliterated terms* used ................................................... 8 7 Risk assessments
    [Show full text]
  • RESUME BORIS ANATOLYEVICH VOLKOVOY Moscow
    RESUME BORIS ANATOLYEVICH VOLKOVOY Moscow Tel/Fax: +7 499 133 7205 Mobile phone: +7 916 113-1469 E-mail: [email protected] EDUCATION: Moscow State University, College of Linguistics MA, 1992, English and French major Moscow Oil and Gas University. A one year training course in industrial safety and HSE for Oil and Gas Industry (2008-2009) Native languages: Russian and Ukrainian EXPERIENCE: 1990 / MD-Seis Joint Enterprise : Raduzhny, interpreter 1991 / White Nights Joint Venture : Raduzhny, interpreter 1991 - 1992 / Dowell-Schlumberger : Moscow - Raduzhny , coordinator 1992 / Technology Ventures ; Raduzhny, Surgut, Nizhnevartovsk, Tengiz, Orenburg; interpreter 1992-1993 / Chevron : Tengiz , interpreter 1993 / Halliburton : Nizhnevartovsk , Arkhangelsk , Usinsk , interpreter 1994 / Brown and Root : Moscow , Arkhangelsk , Ashkhabad , translator and interpreter 1994 / Houston Engineers : Nizhnevartovsk , Megion , Surgut , interpreter 1994 / Statoil : Moscow ; interpreter 1994 / Camco Drilling Group (Reed, Hycalog): Nizhnevartovsk, Nefteugansk, Murmansk, Ashkhabad, Baku ; 1995 / REDA Pump Co. ; Raduzhny; interpreter 1995 / Agip SpA ; Kogalym, Langepas, Moscow; interpreter/translator 1995 / Alfa Laval Oilfield Services ; translating of technical manuals 1995 / Occidental Petroleum ; Baku; interpreter 1995 / Stewart & Stevenson ; Megion ; Langepas ; interpreter 1996-1997 / Exxon Ventures CIS ; Moscow, Kazakhstan, Sakhalin ; translator and interpreter 1996 / British Gas/Agip ; Karachaganak ; interpreter 1996 / Total ; Moscow, Kharyaga ; translation
    [Show full text]
  • Bank of Khanty Mansiysk
    Издательский проект Publishing project Международный институт проблем The international institute of problems of Международного института проблем The international institute of problems of устойчивого развития sustainable development устойчивого развития sustainable development ¿Í͉ËÚÓ‚‡Ì ÔË Œ„‡ÌËÁ‡ˆËË Œ·˙‰ËÌÂÌÌ˚ı Õ‡ˆËÈ Accredited by the United Nations ÃÂʉÛ̇ӉÌ˚È ËÌÒÚËÚÛÚ ÔÓ·ÎÂÏ ÛÒÚÓÈ˜Ë‚Ó„Ó ‡Á- The international institute of problems of sustain- »Á‰‡ÂÚÒˇ ÔË ËÌÙÓχˆËÓÌÌÓÈ ÔÓ‰‰ÂÊÍ Published with information support of the Ministry of For- ‚ËÚˡ (ûœ”–) ÔÓ‚Ó‰ËÚ ‡·ÓÚ˚ ÔÓ ÙÓÏËÓ‚‡Ì˲ ûƒ –ÓÒÒËË eign Affairs of Russia able development (IIPSD) carries out works on the for- ‚ –ÓÒÒËÈÒÍÓÈ ‘‰‡ˆËË Ì‡Û˜ÌÓ-ÏÂÚÓ‰ÓÎӄ˘ÂÒÍÓÈ √·‚Ì˚È Â‰‡ÍÚÓ Editor in chief mation in the Russian Federation of a scientific-method- ·‡Á˚, ‚ÌÛÚË„ÓÒÛ‰‡ÒÚ‚ÂÌÌÓÈ Ë ÏÂʉÛ̇ӉÌÓÈ ÒË- ÇÍÒËÏ ¿ÎÂÍ҇̉ӂ˘ ‘≈ƒŒ–≈ÕüŒ Maxim FEDORENKO ological base, the state and international system of co- [email protected] [email protected] ÒÚÂÏ ÒÓÚÛ‰Ì˘ÂÒÚ‚‡ ‰Îˇ ‡ÎËÁ‡ˆËË ÔÓ„‡ÏÏ ÛÒ- operation for the realization of programmes of sustain- –‰‡ÍÚÓ Editor ÚÓÈ˜Ë‚Ó„Ó ‡Á‚ËÚˡ. ¬ËÍÚÓ ¿ÎÂÍ҇̉ӂ˘ ÿÀ‹÷≈¬ Victor MALTSEV able development. [email protected] [email protected] Дирекция МИПУР Directorate of IIPSD ‡ÎËÁÛÂÚ ÒÚ‡Ú„˲ ûœ”– ̇ ÛÒÚÓȘ˂Ó Зарубежные представительства журнала Foreign representatives of the magazine, realizes the strategy of IIPSD on sustainable ‡Á‚ËÚË ‚ ÍÓÌÍÂÚÌ˚ı ÔÓÂÍÚ‡ı; ‡Á‡·‡Ú˚‚‡ÂÚ «Внешнеэкономические связи» и Международного ‘External Economic Relations’ and The International Insti development in concrete projects; develops института проблем устойчивого развития tute of sustainable development problems ÏÂı‡ÌËÁÏ˚ Ë ÔË‚ÎÂ͇ÂÚ ÚÂıÌÓÎÓ„ËË, mechanisms and involves the technologies Ó·ÂÒÔ˜˂‡˛˘Ë ÛÒÚÓȘ˂Ó ‡Á‚ËÚË √ÂχÌˡ: „.
    [Show full text]
  • Geological Excursion BASE-Line Earth
    Geological Excursion BASE-LiNE Earth (Graz Paleozoic, Geopark Karavanke, Austria) 7.6. – 9.6. 2016 Route: 1. Day: Graz Paleozoic in the vicinity of Graz. Devonian Limestone with brachiopods. Bus transfer to Bad Eisenkappel. 2. Day: Visit of Geopark Center in Bad Eisenkappel. Walk on Hochobir (2.139 m) – Triassic carbonates. 3. Day: Bus transfer to Mezica (Slo) – visit of lead and zinc mine (Triassic carbonates). Transfer back to Graz. CONTENT Route: ................................................................................................................................... 1 Graz Paleozoic ...................................................................................................................... 2 Mesozoic of Northern Karavanke .......................................................................................... 6 Linking geology between the Geoparks Carnic and Karavanke Alps across the Periadriatic Line ....................................................................................................................................... 9 I: Introduction ..................................................................................................................... 9 II. Tectonic subdivision and correlation .............................................................................10 Geodynamic evolution ...................................................................................................16 Alpine history in eight steps ...........................................................................................17
    [Show full text]
  • Balkatach Hypothesis: a New Model for the Evolution of the Pacific, Tethyan, and Paleo-Asian Oceanic Domains
    Research Paper GEOSPHERE Balkatach hypothesis: A new model for the evolution of the Pacific, Tethyan, and Paleo-Asian oceanic domains 1,2 2 GEOSPHERE, v. 13, no. 5 Andrew V. Zuza and An Yin 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, California 90095-1567, USA doi:10.1130/GES01463.1 18 figures; 2 tables; 1 supplemental file ABSTRACT suturing. (5) The closure of the Paleo-Asian Ocean in the early Permian was accompanied by a widespread magmatic flare up, which may have been CORRESPONDENCE: avz5818@gmail .com; The Phanerozoic history of the Paleo-Asian, Tethyan, and Pacific oceanic related to the avalanche of the subducted oceanic slabs of the Paleo-Asian azuza@unr .edu domains is important for unraveling the tectonic evolution of the Eurasian Ocean across the 660 km phase boundary in the mantle. (6) The closure of the and Laurentian continents. The validity of existing models that account for Paleo-Tethys against the southern margin of Balkatach proceeded diachro- CITATION: Zuza, A.V., and Yin, A., 2017, Balkatach hypothesis: A new model for the evolution of the the development and closure of the Paleo-Asian and Tethyan Oceans criti- nously, from west to east, in the Triassic–Jurassic. Pacific, Tethyan, and Paleo-Asian oceanic domains: cally depends on the assumed initial configuration and relative positions of Geosphere, v. 13, no. 5, p. 1664–1712, doi:10.1130 the Precambrian cratons that separate the two oceanic domains, including /GES01463.1. the North China, Tarim, Karakum, Turan, and southern Baltica cratons.
    [Show full text]
  • Materials) Provided to Shareholders in Preparation for the Annual General Shareholders’ Meeting of Pjsc Gazprom in 2018
    INFORMATION (MATERIALS) PROVIDED TO SHAREHOLDERS IN PREPARATION FOR THE ANNUAL GENERAL SHAREHOLDERS’ MEETING OF PJSC GAZPROM IN 2018 Saint Petersburg, 2018 2 List of information (materials) provided to shareholders in preparation for the annual General Shareholders’ Meeting of PJSC GAZPROM 1. Announcement of the annual General Shareholders’ Meeting of PJSC GAZPROM. 2. PJSC GAZPROM Annual Report for 2017 and Annual Accounts (Financial Statements) for 2017, including the Auditor’s Report. 3. Report on PJSC GAZPROM related party transactions made in 2017. 4. Opinion of PJSC GAZPROM Audit Commission on reliability of data contained in PJSC GAZPROM Annual Report for 2017, Annual Accounts (Financial Statements) for 2017 and in the Report on PJSC GAZPROM related party transactions made in 2017. 5. Review of PJSC GAZPROM Auditor’s Report by the Audit Committee of PJSC GAZPROM Board of Directors. 6. Profit allocation recommendations of PJSC GAZPROM Board of Directors, in particular, the amount, timing and form of payment of the annual dividends on the Company’s shares and the date, as of which the persons entitled to the dividends are determined. 7. Information on the candidacy for PJSC GAZPROM Auditor. 8. Proposals on the amount of remuneration to members of PJSC GAZPROM Board of Directors. 9. Proposals on the amount of remuneration to members of PJSC GAZPROM Audit Commission. 10. Draft Amendments to the Regulation of General Shareholders’ Meeting of PJSC GAZPROM and the comparative table of amendments thereto vs the current version. 11. Information on candidates to PJSC GAZPROM Board of Directors, in particular, on the availability of their consent to be elected.
    [Show full text]
  • Workers' Alliance Against Forced Labour and Trafficking
    165˚W 150˚W 135˚W 120˚W 105˚W 90˚W 75˚W 60˚W 45˚W 30˚W 15˚W 0˚ 15˚E 30˚E 45˚E 60˚E 75˚E 90˚E 105˚E 120˚E 135˚E 150˚E 165˚E Workers' Alliance against Forced Labour and Tracking Chelyuskin Mould Bay Grise Dudas Fiord Severnaya Zemlya 75˚N Arctic Ocean Arctic Ocean 75˚N Resolute Industrialised Countries and Transition Economies Queen Elizabeth Islands Greenland Sea Svalbard Dickson Human tracking is an important issue in industrialised countries (including North Arctic Bay America, Australia, Japan and Western Europe) with 270,000 victims, which means three Novosibirskiye Ostrova Pond LeptevStarorybnoye Sea Inlet quarters of the total number of forced labourers. In transition economies, more than half Novaya Zemlya Yukagir Sachs Harbour Upernavikof the Kujalleo total number of forced labourers - 200,000 persons - has been tracked. Victims are Tiksi Barrow mainly women, often tracked intoGreenland prostitution. Workers are mainly forced to work in agriculture, construction and domestic servitude. Middle East and North Africa Wainwright Hammerfest Ittoqqortoormiit Prudhoe Kaktovik Cape Parry According to the ILO estimate, there are 260,000 people in forced labour in this region, out Bay The “Red Gold, from ction to reality” campaign of the Italian Federation of Agriculture and Siktyakh Baffin Bay Tromso Pevek Cambridge Zapolyarnyy of which 88 percent for labour exploitation. Migrant workers from poor Asian countriesT alnakh Nikel' Khabarovo Dudinka Val'kumey Beaufort Sea Bay Taloyoak Food Workers (FLAI) intervenes directly in tomato production farms in the south of Italy. Severomorsk Lena Tuktoyaktuk Murmansk became victims of unscrupulous recruitment agencies and brokers that promise YeniseyhighN oril'sk Great Bear L.
    [Show full text]
  • Arctic Marine Aviation Transportation
    SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Response CapacityandSustainableDevelopment Arctic Transportation Infrastructure: Transportation Arctic 3-6 December 2012 | Reykjavik, Iceland 3-6 December2012|Reykjavik, Prepared for the Sustainable Development Working Group Prepared fortheSustainableDevelopment Working By InstituteoftheNorth,Anchorage, Alaska,USA PROCEEDINGS: 20 Decem B er 2012 ICElANDIC coast GuARD INSTITuTE OF ThE NORTh INSTITuTE OF ThE NORTh SARA FRENCh, WAlTER AND DuNCAN GORDON FOundation Table of Contents Introduction ................................................................................ 5 Acknowledgments ......................................................................... 6 Abbreviations and Acronyms .......................................................... 7 Executive Summary ....................................................................... 8 Chapters—Workshop Proceedings................................................. 10 1. Current infrastructure and response 2. Current and future activity 3. Infrastructure and investment 4. Infrastructure and sustainable development 5. Conclusions: What’s next? Appendices ................................................................................ 21 A. Arctic vignettes—innovative best practices B. Case studies—showcasing Arctic infrastructure C. Workshop materials 1) Workshop agenda 2) Workshop participants 3) Project-related terminology 4) List of data points and definitions 5) List of Arctic marine and aviation infrastructure AlASkA DepartmENT OF ENvIRONmental
    [Show full text]
  • West Siberian Plain As a Late Glacial Desert
    Quaternary International 237 (2011) 45e53 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint West Siberian Plain as a late glacial desert A.A. Velichko a,*, S.N. Timireva a, K.V. Kremenetski b, G.M. MacDonald b, L.C. Smith b a Institute of Geography, Russian Academy of Sciences, Staromonetny, 29, Moscow 109027, Russia b University of California, Los Angeles, CA 90095-1524, USA article info abstract Article history: The paper presents results of morphoscopic studies of quartz grains recovered from sands underlying Available online 18 January 2011 surficial peat over the West Siberian Plain. The field materials were collected in the course of the RussianeAmerican expedition in 1999e2001. The data obtained proved the existence of a vast area in West Siberia similar to cold deserts in appearance at the late glacial time (and probably even as early as the Last Glacial Maximum e 18e20 ka BP). The desert was confined to the arctic and temperate belts, the southernmost part of the plain being an area of loess accumulation. Ó 2011 Elsevier Ltd and INQUA. All rights reserved. 1. Introduction northern and central regions; sands are found not only in fluvial (terrace) sequences, but also on higher levels including the main At the present stage of the geosphere evolution, West Siberia is divide, the ridge of Siberian Uvals. As the sands occur at the base of the largest area of wetlands (including bogs, marshes and peatlands peats, it was of particular interest to study more fully their genetic in the Northern Hemisphere, just as Amazonia is in the Southern properties, to reconstruct environments at the time immediately Hemisphere).
    [Show full text]
  • FURTHER READING for the Article 'Orogenic Belts' by A. M. C. Şengör
    FURTHER READING for the article ‘Orogenic Belts’ by A. M. C. Şengör in the second edition of the Encyclopaedia of Solid Earth Geophysics published by Springer Cham., Berlin and Heidelberg. Aaron, J. M., editor, 1991, An Issue dedicated to Aspects of the Geology of Japan, Site of the 29th International Geological Congress: Episodes, v. 14, no. 3, pp. 187- 302. Akbayram, K., , Şengör, A. M. C. and Özcan, E, 2017, The evolution of the Intra- Pontide suture: Implications of the discovery of late Cretaceous–early Tertiary mélanges, in Sorkhabi, R., editor, Tectonic Evolution, Collision, and Seismicity of Southwest Asia— In Honor of Manuel Berberian’s Forty-Five Years of Research Contributions: Geological Society of America Special Paper 525, pp. 573-612. Altunkaynak, Ş., 2007, Collision-driven slab breakoff magmatism in northWestern Anatolia, Turkey: The Journal of Geology, v. 115, pp. 63-82. Anonymous, 1984, Origin and History of Marginal and Inland Seas: Proceedings of the 27th International Geological Congress, Moscow, 4-14 August 1984,v. 23, VNU Science Press, Utrecht, vii+223 pp. Arai, R., IWasaki, T., Sato, H., Abe, S. and Hirata, N., 2009, Collision and subduction structure of the Izu–Bonin arc, central Japan, revealed by refraction/wide-angle reflection analysis: Tectonophysics, v. 475, pp. 438-453. Aramaki, S. and Kushiro, I., editors, 1983, Arc Volcanism: Elsevier, Amsterdam, VII+652 pp. Arkle, J. C., Armstrong, P. A., Haeussler, P. J., Prior, M. G., Harman, S., Sendziak, K. L. and Brush, J. A., 2013, Focused exhumation in the syntaxis of the Western Chugach Mountains and Prince William Sound, Alaska: Geological Society of America Bulletin, v.
    [Show full text]
  • 14912441.Pdf
    Khants' Time Hanna Snellman KIKIMORA PUBLICATIONS Series B: 23 Helsinki 2001 © 2001 Aleksanterl Institute © Hanna Snellman ©All photographs by U.T. Sirelius,The National Board of Antiquities Khants' Time ISBN 951-45-9997-7 ISSN 1455-4828 Aleksanteri Institute Graphic design: Vesa Tuukkanen Gummerus Printing Saarijärvi 2001 Table of Content FOREWORD 5 1. INTRODUCTION 7 1.1. Studying the Khants 7 1.2. Sirelius as a Fieldworker 13 1.3. Fieldwork Methodology 20 1.4. Investigating Time 34 2. METHOD OF RECORDING TIME 39 2.1. The Vernacular Calendar 39 2.2. The Christian Calendar 95 2.3. The Combination of the Vernacular and Russian Calendars 104 3. FOLK HISTORY 133 3.1. In the Old Days 138 3.2. From the Russians 141 3.3. After the Forest Fires 144 4. WHEN THE LEAVES ARE FALLING 149 BIBLIOGRAPHY 163 Foreword I started working on this book in August 1998. Almost two years had passed after my dissertation on the lumberjacks of Finnish Lapland. I was still occupied with forest history, but I knew that in order to develop as a scientist, I had to leave the familiar ri­ vers and fells of Finnish Lapland, and do research on something else. Professor Juhani U.E. Lehtonen at the University of Helsinki gave me a hint: there are copies of fieldwork notes written by U.T. Sirelius in our archive. Give them a look, Lehtonen advised me, no doubt with the hope that his student would not ignore one of the emphases of the ethnology department's activities, issues concerning Finno-Ugric peoples, including therefore both East Europe and Russia.
    [Show full text]
  • Subject of the Russian Federation)
    How to use the Atlas The Atlas has two map sections The Main Section shows the location of Russia’s intact forest landscapes. The Thematic Section shows their tree species composition in two different ways. The legend is placed at the beginning of each set of maps. If you are looking for an area near a town or village Go to the Index on page 153 and find the alphabetical list of settlements by English name. The Cyrillic name is also given along with the map page number and coordinates (latitude and longitude) where it can be found. Capitals of regions and districts (raiony) are listed along with many other settlements, but only in the vicinity of intact forest landscapes. The reader should not expect to see a city like Moscow listed. Villages that are insufficiently known or very small are not listed and appear on the map only as nameless dots. If you are looking for an administrative region Go to the Index on page 185 and find the list of administrative regions. The numbers refer to the map on the inside back cover. Having found the region on this map, the reader will know which index map to use to search further. If you are looking for the big picture Go to the overview map on page 35. This map shows all of Russia’s Intact Forest Landscapes, along with the borders and Roman numerals of the five index maps. If you are looking for a certain part of Russia Find the appropriate index map. These show the borders of the detailed maps for different parts of the country.
    [Show full text]