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Hsu shu-cheng and the cancellation of self-government in outer mongoliaHoward-Gibbon, John Edward January 1971 (has links)
This paper outlines the background to the internal conflicts in the Peking government and the Outer Mongolian government in 1919, and relates how these conflicts influenced the negotiations for the cancellation of self-government. In conjunction with this background the translation and analysis of the 1919 section of Hsu She-cheng's nien-p’u provide a fairly detailed picture of the events in Urga in the latter months of 1919. / Arts, Faculty of / Asian Studies, Department of / Graduate
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外蒙問題之研究LI, Biyun 18 June 1937 (has links)
No description available.
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Evolution of the Lower Cretaceous Chifeng Half-Graben Basins, Inner Mongolia, ChinaFriedman, Scott Joshua 01 May 2009 (has links)
As a result of complex extensional tectonics in northeast China and southern portions of Mongolia, some workers have interpreted the Cretaceous Maanshan Uplift and associated Chifeng basins as metamorphic core complex. Previous work has relied solely upon kinematic indicators to determine the structural origin of these basins. To fully understand the creation of these basins, the sedimentiological record was analyzed in this study. The early Cretaceous sedimentary fill of these basins was analyzed to determine if it is synextensional in nature, and if so what manner of extension was in progress during that deposition. The Chifeng basins are filled with four distinct facies associations and are floored by Late Jurassic and Early Cretaceous volcanics of intermediate and felsic composition. The facies associations observed are interpreted as lacustrine/fluvial deposits, alluvial fan conglomerates, distal fan deposits with fluvial deposits, and hanging wall derived fluvial deposits. These facies are composed of sediment shed from the footwall and hanging wall of the master faults and volcanic deposits. Paleocurrent indicators, primarily in the form of imbrication, along with clast count data show provenance directly off the structure separating the two basins and from the eastern margin of the southeast basin. The distribution of facies, as well as paleocurrent data, provenance data, and structural geometry, implies that these basins are of half-graben origin and that no sedimentological evidence exists of an Early Cretaceous metamorphic core complex near Chifeng.
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Household and Gender Dynamics in Pastoral MongoliaGolubski, Alexander 19 November 2019 (has links)
No description available.
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INFLATION TARGETING IN MONGOLIA: A VAR MODEL ANALYSISNergui, Anujin 01 December 2022 (has links)
This study aims to conduct a descriptive analysis of inflation targeting in Mongolia. In this context, I will assess whether the current inflation targeting practice of Mongolia is classified as a fully-fledged, eclectic, or inflation targeting lite regime. Then I will verify that Mongolia validates the prerequisites necessary for the implementation of fully fledged inflation targeting. Finally, I will proceed to a VAR model analysis aiming to describe the determinants of inflation. The results show that the inflation targeting practice of Mongolia falls in inflation targeting lite countries categorization and most of the prerequisites to adopt fully fledged inflation targeting have not been fulfilled. It would require significant improvement in the independence of the Bank of Mongolia’s operation and monetary policy decision making, modeling capabilities within the Bank of Mongolia, and financial stability. Finally, the VAR model results show a relationship among the variables, CPI, money supply, exchange rate, and GDP in Mongolia. The principal finding is that the money supply and exchange rate are more important in explaining variation in CPI than GDP in Mongolia.
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An Internship in Conservation Biology with Craighead Beringia SouthGlover, Alicia Marie 07 September 2010 (has links)
No description available.
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Diet and death in times of war: isotopic and osteological analysis of mummified human remains from southern MongoliaTurner, B.L., Zuckerman, M.K., Garofalo, E.M., Wilson, Andrew S., Kamenov, G.D., Hunt, D.R., Amgalantugs, T., Frohlich, B. 10 1900 (has links)
No / This study presents the results of an isotopic analysis of nine naturally mummified individuals—three adults, two adolescents, one juvenile, and three infants—recovered from the Hets Mountain Cave site in southern Mongolia, where they had been secondarily deposited. All of the individuals show evidence of violent perimortem trauma, but no skeletal indicators of nutritional or disease-related stress. Multi-isotopic data (δ13C, δ15N, δ18O, 87Sr/86Sr, and 20nPb/204Pb) were characterized in multiple tissues from each individual when possible, in order to reconstruct diet composition and residential origin at different points in life. Specifically, δ13C and δ15N in bone carbonate and collagen (N = 8) and hair keratin (N = 4) were coupled with enamel carbonate δ18O and δ13C (N = 3) and enamel 87Sr/86Sr, and 20nPb/204Pb (N = 3) to assess diet and residential mobility in relation to skeletal indicators of health and trauma. Results are consistent with a persistence of mixed C3/C4 pastoral subsistence and general stability of diet composition over the life course, in contrast to contemporary accounts of widespread famine and a dependence on grains imported from China throughout the region. However, results also suggest that at least some individuals may have migrated to this region of southern Mongolia from elsewhere during life, meaning that their dietary isotopic profiles may not represent local subsistence patterns near the Hets Mountain Cave site. Overall, these results speak to the utility of life course oriented multi-isotopic analysis in complementing more top-down historical analyses in understanding variation in subsistence, nutrition, and migration in regions undergoing significant political and economic turmoil.
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Nomadic geography : pastoral environments in the Gobi Desert, MongoliaSternberg, Troy January 2009 (has links)
Pastoralism on the Mongolian steppe encompasses limited physical resources and evolving anthropogenic influences. Little-studied, the Inner Asian region encounters changing climates, evolving land use practices, and socio-economic transition that impact the natural and human geography. This thesis investigates how bio-physical factors and herder action determine the pastoral environment in the Gobi Desert, Mongolia. Research, focusing on drought, degradation and the extreme winter conditions that define pastoralism in Mongolia, examines pastoralists' perception of and interaction with their environment. This approach highlights steppe ecological and social processes within the global dryland debate. Fieldwork in Omnogovi and Ovorhangai Province established that drought is endemic in the region. However, drought events were independent of extreme winter conditions and did not exacerbate their impact. Degradation was not found at water points as vegetation cover decreased with distance from water. While remote sensing showed a decline in vegetation cover over time, it did not establish desertification on the steppe. Changing physical, socio-economic, and political conditions since 1990 continue to impact Mongolian pastoralism. Environmental conditions, particularly water resources and pasture quality, were paramount herder concerns. This research showed that pastoralists are economically motivated, differentiate on multiple dimensions, and value communal land stewardship. On the steppe, traditional mobile livestock practices improve livelihoods and remain an effective management approach. However, the future of pastoralism is uncertain as herders settle, the population ages, and children become educated. Thesis results emphasize the interaction of physical and social environments will define pastoralism's role in the Gobi Desert
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OSL dating of palaeoshorelines of saline lakes at Inner MongoliaNg, Sin-pan., 吳善斌. January 2011 (has links)
published_or_final_version / Applied Geosciences / Master / Master of Science
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Tree-Ring-Derived Precipitation Records From Inner Mongolia, China, Since A.D. 1627Liu, Yu, Sun, Junyan, Yang, Yinke, Cai, Qiufang, Song, Huiming, Shi, Jiangfeng, An, Zhisheng, Li, Xuxiang 06 1900 (has links)
Two Chinese pine (Pinus tabulaeformis) tree-ring width chronologies up to 375 years long were used to reconstruct rainfall from February to early July for the Wu Dangzhao region and from February to mid-July for the La Madong region, Inner Mongolia, China. The predictor variables account for 44.3% and 42.7% of the variance in precipitation, respectively. Both historical records and two other tree-ring based precipitation reconstructions from the environmentally sensitive zone (the northern Helan Mountain range and Baiyinaobao) confirm our results. After applying a 10-year moving average, the trends of four tree-ring based precipitation reconstructions vary synchronously. Periods with below-normal precipitation occurred
during the 1720s–1730s, 1740s–1750s, 1790s, early 1810s, late 1830s–1860s, 1880s–1910s, late 1920s–1930s and after the late 1960s–early 1970s. Periods with above-normal precipitation occurred in the 1760s to early 1770s, 1820s to early 1830s, 1870s–1880s, early 1920s, 1940s to early 1960s, and 1990s. The late 1920s period was the most severe drought over a broad area in north China in the last 375 years. In contrast, the wettest period was in the late 1990s.
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