Academic literature on the topic 'Siberia (Province)'

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Journal articles on the topic "Siberia (Province)"

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Sartor, Valerie, and Svetlana Bogdanova. "Evolving and adapting to global changes regarding English: English language teaching in the Siberian city of Irkutsk." English Today 31, no. 2 (May 28, 2015): 5–10. http://dx.doi.org/10.1017/s0266078415000048.

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The Russian Federation, established after the breakup of the USSR in the early 1990s, is the largest country in the world (Blinnikov, 2011). Russians have long considered their capital, Moscow, and the adjoining city of St Petersburg, to be the centres of culture and commerce, as well of the arts and educational facilities. Due to the large size of their country, Russians designate areas west of the Ural Mountains informally as “European Russia.” The Russian territories known as Siberia and the Russian Far East extend east of the Urals to the Pacific Ocean, and cover approximately 10% of the world's land mass (Yudin, 2006). In May 2000, President Putin designated nine federal subjects (provinces and republics) of Siberia as the Siberian Federal District (http://russiatrek.org/siberia-district). The capital of Irkutsk, located in Irkutsk Province, is situated in the southeastern part of the Siberian Federal District.
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žigaitė, živilė, Valentina Karatajūtė-Talimaa, and Alain Blieck. "Vertebrate microremains from the Lower Silurian of Siberia and Central Asia: palaeobiodiversity and palaeobiogeography." Journal of Micropalaeontology 30, no. 2 (September 1, 2011): 97–106. http://dx.doi.org/10.1144/0262-821x11-016.

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Abstract. The biostratigraphic and palaeogeographical distributions of early vertebrate microfossils from a number of Lower Silurian localities in northwestern Mongolia, Tuva and southern Siberia were reviewed. Vertebrate microremains showed high taxonomic diversity, comprising acanthodians, chondrichthyans, putative galeaspids, heterostracans, mongolepids, tesakoviaspids, thelodonts and possible eriptychiids. The majority of taxa have lower stratigraphic levels of occurrence compared to other Silurian palaeobiogeographical provinces, such as the European-Russian or Canadian Arctic. Vertebrate microremains are numerous within the samples, which may indicate warm-water low-latitude palaeobasins with rich shelf faunas. This disagrees with the recent interpretations of the territory as a northern high-latitude Siberian palaeocontinent. The palaeobiogeographical distribution of vertebrate taxa indicates an endemic palaeobiogeographical province of connected epeiric palaeoseas with external isolation during the early Silurian. In previous works separation between Tuvan and Siberian palaeobiogeographical provinces has been suggested. After careful revision of the vertebrate microfossil record of the region, we find that differences in a few vertebrate taxa do not provide not strong enough evidence to reliably distinguish these provinces. We therefore dispute the hypothesis of two biogeographical provinces in the early Silurian of the Siberian palaeocontinent, and propose a single unified Siberian–Tuvan palaeobiogeographical province.
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Karchaeva, T. G. "ORGANIZATION OF NOTARY BUSINESS IN SIBERIA BEFORE 1896: THE YENISEI PROVINCE." Bulletin of Kemerovo State University, no. 1 (April 25, 2018): 39–45. http://dx.doi.org/10.21603/2078-8975-2018-1-39-45.

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The current paper features organization and operation of notaries in Siberia before 1896. The data obtained have revealed that the Statute of Notaries reached Siberia some thirty years after it had been issued in Central Russia in 1866. The article contains information about the development of the history of Notarial Institute in the Yenisei province before and after the Siberian Notary Reform of 1896. It has been concluded that Siberia had regional peculiarities in its management in the pre-revolutionary period of Russian history. In the XVIII century notary functions were performed by clerks, bailiffs and "weeklings", after 1822 – by officials of city councils and police employees (e.g. the city of Turukhansk). The author notes that the rapid social and economic changes in Siberia predetermined the need for the development of the pre-reform notary as an independent legal institution. Archival materials reveal that the first notary began his work in Krasnoyarsk as late as in 1883, and he was not a state servant, the way it was in Central Russia, but was elected by the local municipal authorities; what is more, neither authorities nor society had any influence on his activities. It was concluded that the pre-1896 Siberian notaries had a number of regional features that played their role in the pre-revolutionary period of Russian history.
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Suslova, L. N., I. V. Yarkova, and R. G. Bukanova. "Everyday Life of Population of Siberian Province in Context of Peter’s I Reforms in First Quarter of 18th Century." Nauchnyi dialog, no. 6 (June 24, 2021): 448–66. http://dx.doi.org/10.24224/2227-1295-2021-6-448-466.

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The article is devoted to the study of the evolution of the culture of everyday life of the Siberian province population in the first quarter of the 18th century, the characteristics of the development of traditional forms of material culture of Siberians, and new features of everyday life that arose under the influence of the implementation of Peter's reforms on the territory of Western Siberia. Changes in the material culture, leisure and life of the population of the Siberian province in the first quarter of the 18th century are considered, the traditions of building houses, making clothes, the level of medical care and health care, leisure activities of the population of Western Siberia in the first quarter of the 18th century are described. The study was carried out on the basis of an analysis of the complex of legislative and office-work sources of the State Archives in Tobolsk. Among them, an important place is occupied by decrees regulating the organization of medical care for the population, documents reflecting the actions of local authorities in relation to the occupation of Swedish prisoners of war in Tobolsk by distilling. The authors of the article show that Peter's modernization processes in the field of culture, customs and everyday life had little effect on the traditions of building houses, making clothes, and everyday activities of the majority of the peasant population of the Siberian province and local non-Russian peoples. It is concluded that the main changes affecting the area of everyday culture are associated with the implementation of the military and administrative reforms of Peter I, the appearance of captured Swedes on the territory of the province, the implementation of the provincial reform, a change in the local administration system, the emergence of medical professional personnel and health care institutions.
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Antipova, E. M. "THE STRUCTURE OF THE SIBERIAN GEOGRAPHICAL FLORAL ELEMENT IN THE MIDDLE SIBERIAN FOREST STEPPES." Proceedings on applied botany, genetics and breeding 180, no. 3 (October 29, 2019): 76–81. http://dx.doi.org/10.30901/2227-8834-2019-3-76-81.

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Background. The ultimate goal of studies of any flora is the clarification of the history of vegetation cover and individual taxa formation in the studied region, determination of the degree of its individuality, of floristic links with other territories, and of regularities in flora formation.Materials and methods. The flora of vascular plants in the island forest steppes of Middle Siberia, i. e. of the Krasnoyarsk, Kansk and Achinsk forest steppes, identified by the specific floras method of A. I. Tolmachev, was chosen as the object of research. The purpose of the paper was to study the structure of the Siberian geographical element in the steppe flora, characteristics of the types of constituent distribution areas selected on the basis of the phytochorion concept. The basis for determining the types of habitats was the planetary regionalization scheme by A. L. Takhtajan, complemented by statistical convergent zonation for Siberia by L. I. Malyshev, and for the Russian Far East by R. V. Kamelin.Results. The territory of the Middle Siberian forest steppes is a part of the Altai-Yenisei Province. The Krasnoyarsk, Kansk and Achinsk forest steppes (Krasnoyarsk Territory) are the most northern parts of the region (55°28’–57°28’N, 89°– 96°40’E). Twenty-six local floras were examined. Ten distribution area types were identified within the Siberian geographical element of the boreal group according to the names of sub-regions and provinces (154 species, 11.12%), limiting their distribution from West to East or from East to West, including all intermediate Siberian provinces between them. All types of distribution areas were combined into four large subgroups, namely Siberian, West Siberian, Middle Siberian, and East Siberian. Names of geographical elements were composed from the names of several phytochoria, in which they had been registered, according to the rules by M. G. Popov.Conclusions. The Siberian geographical element rates third in all three forest steppes after the Euro-Siberian and Circumboreal geographical elements. In the flora of the Middle Siberian forest steppes Siberian elements amount to 11%, among which the Middle Siberian ones prevail (4.4%, 61 species) due to the geographical position of the flora. The fraction of species distributed throughout Siberia is 3.25% (45 species), followed by East Siberian species (2.24%, 31 species) and West Siberian ones (1.23%, 17 species).
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Khomentovsky, V. V. "The Vendian System of Siberia and a standard stratigraphic scale." Geological Magazine 123, no. 4 (July 1986): 333–48. http://dx.doi.org/10.1017/s0016756800033422.

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AbstractIn Siberia Vendian is equated with a Yudoma Complex or Yudomian. Yudomian deposits of the Siberian Platform and adjacent geosynclines differ greatly in facies and thickness. According to the composition and structure of Yudomian deposits, four facies provinces may be recognized on the platform. Local stratigraphic charts for each province are presented and their correlation and possibility to subdivide the Vendian System in Siberia into three horizons or stages are substantiated. The upper stage (Nemakit–Daldyn), on the basis of palaeontological evidence, is in its turn subdivided into two zones: Anabarites trisulcatus and Purella antiqua.The most important Early Baikalian rearrangement is proved to take place around 800±50 Ma. The pre-Vendian (Late Baikalian) movements, though less intensive, make the determination of the Yudomian lower boundary easier.The specific character of Vendian biostratigraphy is discussed involving all groups of the organic remains, that causes the necessity of recognition, subdivision and correlation on the basis of the whole complex of data.The boundary between the Vendian System and the Lower Cambrian Tommotian Stage (in type section) is proved to conform to the base of the Pestrozvet Formation, which divides the A. sunnaginicus and P. antiqua zones.
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Cai, Yaoping, Hong Hua, Andrey Yu Zhuravlev, José Antonio Gámez Vintaned, and Andrey Yu Ivantsov. "Discussion of ‘First finds of problematic Ediacaran fossil Gaojiashania in Siberia and its origin’." Geological Magazine 148, no. 2 (September 9, 2010): 329–33. http://dx.doi.org/10.1017/s0016756810000749.

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Y. Cai & H. Hua comment: Zhuravlev, Gámez Vintaned & Ivantsov (2009) reported the problematic Ediacaran fossil Gaojiashania annulucosta in Siberia and they considered that this is the first find of Gaojiashania outside China, since Gaojiashania had previously only been reported from the Gaojiashan Member of the middle Dengying Formation in the Ningqiang area, southern Shaanxi Province, South China. However, we believe that the so-called Siberian Gaojiashania was mis-identified, and what was described as Gaojiashania annulucosta by Zhuravlev, Gámez Vintaned & Ivantsov (2009) is more appropriately ascribed to Shaanxilithes ningqiangensis, another problematic Ediacaran fossil that has also been known from the Gaojiashan Member in Shaanxi Province of South China (Chen, Chen & Lao, 1975; Xing et al. 1984), as well as the stratigraphically equivalent Taozichong Formation in Guizhou Province (Hua, Chen & Zhang, 2004) and the Jiucheng Member (Dengying Formation) in Yunnan Province of South China (Zhu & Zhang, 2005), the Zhoujieshan Formation in Qinghai Province (Shen et al. 2007), and the Zhengmuguan Formation in Ningxia Hui Autonomous Region of North China (Shen et al. 2007).
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Stevens, Calvin H., and Charles A. Ross. "Fusulinids from piston cores, Northwind Ridge, Amerasia Basin, Arctic Ocean." Journal of Paleontology 71, no. 3 (May 1997): 357–60. http://dx.doi.org/10.1017/s0022336000039378.

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Fusulinaceans from the flank of Northwind Ridge in the Arctic Ocean indicate that this feature is underlain by miogeoclinal upper Paleozoic strata, and that the fauna belongs to the Middle Carboniferous through Early Permian Arctic Fusulinacean Province. This province stretched from the Canadian Arctic Islands eastward to Svalbard where it merged with the similar Ural Fusulinacean Province in the western Ural Mountains. Because these provinces did not extend into Siberia, the Northwind Ridge assemblage indicates that these rocks originally were adjacent to, or a part of, the Canadian Arctic Islands Carboniferous-Permian shelf margin.
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Zhuravlev, Andrey Yu. "Evolution of archaeocyaths and palaeobiogeography of the Early Cambrian." Geological Magazine 123, no. 4 (July 1986): 377–85. http://dx.doi.org/10.1017/s0016756800033471.

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AbstractIn the Early Cambrian, there were two peaks of the increase in number of new archaeocyathan genera. These diversification bursts are, perhaps, related to significant changes in Early Cambrian palaeogeography. The first burst at the beginning of the Atdabanian was, perhaps, connected with the initiation of archaeocyathan expansion beyond the Siberian Platform. During the second half of the Atdabanian, closely related archaeocyathan assemblages were established from North Africa to Australia because neither climate, nor geographic isolation could have affected their differentiation in that time. At the end of the Atdabanian and the beginning of the Botomian the number of archaeocyathan genera again increased sharply, and isolated provinces were established. The American–Koryakiyan province was formed in western North America (from Alaska to Sonora) and included the Koryakiya, while the Afro–Siberian–Antarctic province probably extended from North Africa and Western Europe to Siberia, Australia, and Antarctica. The main difference between the regular archaeocyathan assemblages lies in what skeletal elements filled the intervallum. There was a certain stability in the distribution of skeletal elements of high taxonomic rank and an interchangeability of elements of low taxonomic rank.
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Korzhenevsky, K. B. "Territorial Delimitation between Altai, Omsk and Semipalatinsk Provinces in 1925." Nauchnyi dialog, no. 5 (May 28, 2021): 371–83. http://dx.doi.org/10.24224/2227-1295-2021-5-371-383.

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A detailed analysis of the process of demarcation of the Altai province from the Omsk province of the RSFSR and the Semipalatinsk province of the Kirghiz (since June 1925 — Kazak) ASSR, which were first involved in scientific circulation is carried out on the basis of the archival documents. It is shown that it consisted in an attempt by the Altai authorities to withdraw the territory of the Narrow Steppe from under their jurisdiction and transfer it to the adjacent provinces in the first half of 1925. The history of this border issue, which arose as a result of the inclusion of the Korostelevskaya steppe in the Kyrgyz ASSR, is investigated. The course of discussion of changes in the border line between the authorities of the three provinces and Moscow is described. Various arguments proposed by the parties, options for resolving the problem that have arisen are considered; and also, it is explained why, in the end, the disputed border territory remained part of Siberia. It is noted that the attempts of the leadership of the Altai province to transfer part of the territory of the Uglovsky district with the “Narrow Steppe” tract under the control of the Omsk and Semipalatinsk provinces are noted. It is concluded that the issue of the status of the Narrow Steppe during the nationalterritorial demarcation between Siberia and Kazakhstan was one of the most difficult and went beyond the traditional ways of solving similar problems.
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Dissertations / Theses on the topic "Siberia (Province)"

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Anderson, David George. "The social movements of the Zabaikal'skie Evenki state, civil society, and economy in a Siberian Province /." 1991. http://catalog.hathitrust.org/api/volumes/oclc/23855608.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1991.
Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 119-123).
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Books on the topic "Siberia (Province)"

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James, Hughes. Stalinism in a Russian province: Collectivization and dekulakization in Siberia. Basingstoke: Macmillan, 1996.

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James, Hughes. Stalinism in a Russian province: A study of collectivization and dekulakization in Siberia. New York: St. Martin's Press in association with the Centre for Russian and East European Studies, University of Birmingham, 1996.

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Russian world in China // Русский мир в Китае. Moscow, Russia.: Vostochnaya literature, 2013.

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Русский мир в Китае: исторический и культурный опыт сосуществования русских и китайцев. Moscow: Vostochnaya literature, 2013.

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Book chapters on the topic "Siberia (Province)"

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Zakharov, Yuri D., Alexander S. Biakov, Micha Horacek, Ruslan V. Kutygin, Evgeny S. Sobolev, and David P. G. Bond. "Environmental Control on Biotic Development in Siberia (Verkhoyansk Region) and Neighbouring Areas During Permian–Triassic Large Igneous Province Activity." In Morphogenesis, Environmental Stress and Reverse Evolution, 197–231. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-47279-5_10.

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Hughes, James. "The Ural-Siberian Method." In Stalinism in a Russian Province, 73–91. London: Palgrave Macmillan UK, 1996. http://dx.doi.org/10.1057/9780230379985_5.

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Sharma, Mukul. "Siberian Traps." In Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism, 273–95. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm100p0273.

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Rossak, B. T., H. Kassens, H. Lange, and J. Thiede. "Clay Mineral Distribution in Surface Sediments of the Laptev Sea: Indicator for Sediment Provinces, Dynamics and Sources." In Land-Ocean Systems in the Siberian Arctic, 587–99. Berlin, Heidelberg: Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-60134-7_45.

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Latyshev, A. V., N. A. Krivolutskaya, P. S. Ulyahina, Ya V. Bychkova, and B. I. Gongalsky. "Intrusions of the Kulumbe River Valley, NW Siberian Traps Province: Paleomagnetism, Magnetic Fabric and Geochemistry." In Springer Geophysics, 67–82. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90437-5_6.

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Lightfoot, Peter C., and Chris J. Hawkesworth. "Flood Basalts and Magmatic Ni, Cu, and PGE Sulphide Mineralization: Comparative Geochemistry of the Noril'sk (Siberian Traps) and West Greenland Sequences." In Large Igneous Provinces: Continental, Oceanic, and Planetary Flood Volcanism, 357–80. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm100p0357.

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Riasanovsky, Valentin A. "Juristic Customs of the Tartars of Kuznetzk District of the Tomsk Province." In Customary Law of the Nomadic Tribes of Siberia, 47–53. Routledge, 2017. http://dx.doi.org/10.4324/9781315541358-4.

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Hinzman, Larry D., and Leslie A. Viereck. "Climate and Permafrost Dynamics of the Alaskan Boreal Forest." In Alaska's Changing Boreal Forest. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780195154313.003.0008.

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There are large climatic differences among the boreal regions of the world. The extreme continental climates of central Siberia, with a mean annual temperature of –11°C or colder and precipitation of only 150 mm, for example, contrasts strikingly with the semicoastal climate of Newfoundland, with a mean annual temperature of +5°C and precipitation of 1400 mm. Yet both are considered boreal. This wide range in mean annual temperatures translates into large variation in the soil thermal conditions. Although much of the northern region of the boreal forest is underlain by continuous and discontinuous permafrost, southern regions are entirely permafrost-free. Boreal Canada has been classified into four major ecoclimatic provinces (Ecoregions Working Group 1989). The Subarctic Ecoclimatic Province extends from treeline in northern Canada south to the border with continuous stands of closed spruce. It ranges from the highly continental areas of northern Yukon Territory to the wetter and somewhat warmer regions of the Labrador Peninsula. The Boreal Ecoclimatic Province includes the main body of the boreal forests of Canada from the Mackenzie River east to Newfoundland. It is a complicated province that has been divided into High, Mid-, and Low Boreal, with a wide range of climate conditions. The Subarctic Cordilleran Ecoclimatic Province occurs only at higher elevations in western Canada. Forested areas in this region are usually restricted to valley bottoms or low, south-facing slopes. The Cordilleran Ecoclimatic Province includes the mountain ranges along the west coast and the continental divide from Montana to Alaska and from the Yukon River south to the boundary with the coastal forests. The boreal portion of this province has climates similar to that of the eastern section of the Interior Highland Ecoregion of Alaska (Fig. 2.3, Gallant et al. 1995). Alaska does not fit well into these Canadian ecoclimatic provinces because of differences in elevation, the effects of the two east-west-oriented mountain ranges (the Alaska and Brooks Ranges), and the coastal influences of the Bering Sea to the west and Cook Inlet to the south (Fig. 1.1; Hopkins 1959, Hare and Ritchie 1972). Hammond and Yarie (1996) separated Alaska into 35 ecoclimatic regions, of which nine include areas of boreal forest.
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Rigassi, Danilo A. "Wrench Faults as a Factor Controlling Petroleum Occurrences in West Siberia." In Future Petroleum Provinces of the World. American Association of Petroleum Geologists, 1986. http://dx.doi.org/10.1306/m40454c23.

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Verschuur, Gerrit L. "On the Edge of Extinction." In Impact! Oxford University Press, 1996. http://dx.doi.org/10.1093/oso/9780195101058.003.0012.

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On the morning of June 30, 1908, civilization may have suffered the worst piece of luck in its history. A small cometlike object exploded in the atmosphere above the Tunguska river valley in Siberia. It did little more than scorch and flatten trees for 20 kilometers in all directions and kill a thousand reindeer. However, if that object had struck a heavily populated region, we would not now dwell under any illusion concerning how close to the edge of extinction the human species actually hovers. Because the Tunguska missile missed a populated area, the threat of impact did not really begin to enter the public imagination until after the 1980 announcement of the discovery of the iridium in the K/T boundary layer. Had the Tunguska object struck a large city, a million people or more might have perished, and the phenomenon would have raised everyone’s awareness to the threat of comet impact. Instead, nearly a century later, the threat of comet and asteroid impact is regarded as little more than an interesting anecdote. Very slowly the nature of the threat is being recognized, but only because of the somewhat esoteric discovery that the dinosaurs were wiped out by a major impact 65 million years ago. Such huge collisions are infrequent, perhaps about once every 50 to 100 million years. It is the smaller impacts that pose the greatest danger, and they occur far more frequently. About 800 years ago the South Island of New Zealand suffered widespread fires, which leveled the island and led to the extinction of the Moa bird. Maori legend says that a big explosion in the sky was the cause of the strange fire. Duncan Steel of the University of Adelaide and Peter Snow from Otago in New Zealand have pieced together a fascinating scenario that suggests that the Maori were correct. The fireball created by a comet impact may have ignited the forests of South Island. Near the town of Tapanui in the province of Otago there exists a crater that geologists have been slow to identify as extraterrestrial in origin.
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Conference papers on the topic "Siberia (Province)"

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Büyükakıncı, Erhan. "The Siberian Factor in the Russian Foreign Policy: Economic Instruments and Geopolitical Games." In International Conference on Eurasian Economies. Eurasian Economists Association, 2015. http://dx.doi.org/10.36880/c06.01297.

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In this paper, we try to discuss how the Siberian part of the Russian territory can present advantages and disadvantages for Russian foreign policy. Situated in the center of the Eurasian geography, Siberia offers many economic opportunities and energy reserves as well as a strategic value for Russia, whose population and interests are mostly concentrated in the western provinces. Long considered as an isolated continent for exile for political dissidents, Siberia has become nowadays a center of the economic strategies of the Russian administration, in relation with its foreign policy perspectives. As an energy source for natural gas and oil and transit corridor toward China and Kazakhstan, Siberia is now supported through governmental policies of restructuration and labour migration. This new perspective can lead to a new policy of regionalism in connection with foreign policy interests. For the federal center, there is an unavoidable correlation between the domestic and foreign policy stakes with Siberia’s integration in world and regional politics.
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Chayka, Ivan, Vadim Kamenetsky, Yuriy Vasilyev, and Ilya Prokopyev. "SPINEL-GROUP MINERALS IN PERIDOTITES OF THE GULI AND BOR-URYAKH INTRUSIONS (MEIMECHA-KOTUY PROVINCE, NORTHERN SIBERIA)." In 20th SGEM International Multidisciplinary Scientific GeoConference Proceedings 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020/1.1/s01.038.

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Grabovskaya, F. R. "Facial-Cyclostratigrapfic Model of the Berrias-Valangin Structure in Western Siberia (North-East of the Sredneobskaya Oil and Gas Province)." In Saint Petersburg 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800191.

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Chelakova, Yulia, and Oleg Dolgikh. "TECHNOGENIC GEOCHEMICAL PROVINCE OF SOUTHERN SIBERIA AND FEATURES OF THE IMMUNE AND GENETIC STATUS OF THE ADULT POPULATION OF THE REGION." In 20th SGEM International Multidisciplinary Scientific GeoConference Proceedings 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020v/6.2/s08.19.

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Kazanenkov, Valeriy A., and Vasiliy Yu Nemov. "Major directions and tasks of oil and gas searches in Western Siberia for next decades." In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-088.

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The perspective directions for the development of oil production in the West Siberian oil and gas province are substantiated: new for economic development and still poorly studied by deep drilling in the central and northern parts of the Gydansky Peninsula, Yenisei–Khatanga regional trough, and the waters of the southern part Kara Sea with the Ob and Taz bays. A retrospective analysis was performed and the geological data on the open fields of the territory under consideration were summarized.
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Miroshnichenko, D. E. "Sand Reservoirs Characterization Using Multiwave Seismic in West Siberia." In Tyumen 2013 - New Geotechnology for the Old Oil Provinces. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20142720.

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Morozov, P., G. Paton, A. M. Milushkin, V. V. Kiselev, and D. N. Myasoedov. "Application of High Definition Frequency Decomposition Techniques on Western Siberia Reservoirs." In Tyumen 2013 - New Geotechnology for the Old Oil Provinces. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20142716.

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8

Baldin, V. A., R. Y. Adiev, and N. Z. Munasypov. "Western Siberia: Main Directions of Geological Exploration and Development Prospects in the XXI Century." In Tyumen 2013 - New Geotechnology for the Old Oil Provinces. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20142719.

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Davletova, E., K. Zverev, I. Buyakina, and N. Nassonova. "Facies Analysis and Reservoir Properties of Early Cretaceous Beds in Samotlor Field, West Siberia Basin." In Tyumen 2013 - New Geotechnology for the Old Oil Provinces. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20142755.

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Edwards, Felix Alexandre, Benjamin Alexander Black, Anna M. Martini, and David S. Jones. "SOURCES OF MERCURY DURING LARGE IGNEOUS PROVINCE EMPLACEMENT: THE CENTRAL ATLANTIC MAGMATIC PROVINCE AND SIBERIAN TRAPS." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344658.

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Reports on the topic "Siberia (Province)"

1

Petroleum geology and resources of the Baykit High province, East Siberia, Russia. US Geological Survey, 2001. http://dx.doi.org/10.3133/b2201f.

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