This dissertation explores entanglements of body, national identity and nature in contemporary Mongolia. The project is situated within the rising popularity of natural remedies and alternative medicine during a time described as disorganized (zambaraagui) and disorderly. Data was collected from 33 months of fieldwork in Ulaanbaatar and elsewhere, focused on non-biomedical practices and therapeutic landscapes, especially medicinal springs (arshaan) and their sanatoria. This work contributes to studies of post-socialist Mongolia in a few ways. The methodological decision to engage in interview and participant observation of fortunetellers (üzmerch), practitioners of Buddhist and traditional medicine (otoch, ardiin emch), astrologists (zurhaich), energy healers (bio energich), shamans (böö, zairan, udgan), enlightened lamas (huvilgaan) and massage therapists (bariach) was driven by the fluid approach with which patients approach fulfilling the needs of their health and wellbeing. Such fluidity was also echoed in healing practice; as opposed to bounded by strict conceptual distinctions, healers re-purposed personally and culturally-familiar techniques, ranging from biomedical to those of Buddhist medicine (sowa rigpa) to occult practices. Many of the same techniques were practiced by a range of practitioners. The term orthopraxy, commonality of practice across conceptual difference, is used to address this phenomena. Such pairing together of different kinds of therapies – biomedical or otherwise – calls into question a “traditional” vs. modern or neo-spiritual framework within which such practices are often cast. I employ Robbin’s anthropology of discontinuity (2003), suggesting that Soviet influences represented “hard” cultural forms that provided a partial rupture in cultural knowledge between pre-revolutionary society and 1990. Nature (baigal) and natural surroundings (baigal orchin) were concepts often raised when discussing health and wellbeing. “Spiritual” earth and mountain masters (gazariin/uuliin ezed) of estranged homelands (nutag) that cause illness in families relocated to Ulaanbaatar; the water, flora, and mutton from one’s homeland as especially medicinally-suited to the body; shamans empowered to heal by appropriating into their practices the worship of nationally-significant mountains: territorialized national identity represented a prominent trend in healing practices. The revering of a nation through natural landmarks I call national nature, and suggest it be seen both with respect to romantic and utilitarian conceptions of a therapeutic nature that underpinned Soviet medicine, and Soviet indigenization campaigns and the ethnonationalism that was encouraged to flourish in borderland republics. Affective rooting to natural landmarks to maintain or restore wellbeing was also a way to enact Mongol-ness, rendering healing the body at once a practice of national subject-making.

This thesis presents a holistic study of connections in the Altai Mountains of the eastern Eurasian Steppe, as shown by rock-art. Currently divided by four countries, pecked images (petroglyphs) and painted images from the 2^nd-1^st millennium BCE have been subjected to very separate research traditions, exacerbated by language barriers. This thesis focusses on the entire Altai Mountain range as a study area, integrating research published in Chinese and Russian, with supplementary literature in Kazakh and Mongolian consulted. To demonstrate the potential for connectivity and, consequently, movement, a map of accessibility was generated, showing that there are various optimal routes for movement throughout the Altai. The locations of rock-art sites relative to these routes indicate that movement was a key feature contributing to the creation of rock-art. Examining topographic features in the vicinity of rock-art sites of three regions (Mongolia, Russia, PRC) highlighted an association between watercourses and sites, whilst studying the micro-landscape within panels found that the creators of rock-art were not representing the tangible spatial relationship of figures to the landscape. More broadly, similarities between motifs at rock-art sites, as well as on portable art, demonstrate that the people making them, regardless of whether they were aware of it or not, were part of a wider understanding of how to depict subjects. Evidence of this understanding can be found even in regions with very different cultural backgrounds to the Steppe, such as the Chinese Central Plains, demonstrating that groups outside of the Steppe were aware of and using this way of representing. By combining analysis of motifs with that of the landscape, this thesis demonstrates that rock-art as a practice was inherently linked with to the landscape, whereas content and style are more indicative of a wide-ranging belief system amongst Steppe pastoralists, which was expressed aesthetically.

Il est débattue sur le temps closural finale de l'océan paléo-asiatique et la position. Certains géologues ont préconisé la suture "Solonker" marque la zone closural finale du Permien , tandis que d'autres insistent sur le fait Paléozoïque milieu. Nos trois domaines d'étude, le Hongqi , le Ondor Somme et le Mandula ont essentiel et important de résoudre ces controverses. Les unités litho-tectonique reconnus dans le domaine Hongqi-Ondor Sum sont le mélange Belt de Hongqi-Ondor Sum, la Belt de l'arc Bainaimiao, craton du Nord de Chine et les roches sédimentaires post-orogéniques. Le mélange Belt de Hongqi-Ondor Sum connu déformation ductile en deux phases et une phase de la déformation ductile-fragile. D1 est responsable de la S1 foliation, linéation minérale L1, et intrafolial pli F1. Les critères cinématiques indiquent un sens cisaillement de top-to-the-NW. D2 est caractérisée par divers taille de plis asymétriques avec axe presque NE correspondant à la poussée NW cisaillement. D3 formé le cadre régional dans le Hongqi et les zones Ondor Sum. La zone Mandula contient les sédiments olistostrome, les sédiments turbiditiques et roches volcanosédimentaires. Grains de zircons détritiques dans des échantillons sédimentaires indiquent la zone d'étude Mandula reçu des matériaux d'arc Bainaimiao et matières contemporaines de l'éruption volcanique du Permien. Les sédiments et les roches volcaniques dans la région Mandula soumettent un NW-SE ou près de N-S du raccourcissement. Les données géologiques indiquent qu'une subduction et collsion dans Paléozoïque inférieur, et rifting et fermeture rift dans Palezoic supérieur. Les fragments ophiolitiques "Solonker" sont en effet olistostrome. Composants ophiolitiques typiques ne sont pas observés dans la région Mandula. / It is hotly debated about the final closural time and position of the Paleo-Asian Ocean. Some geologists advocated the “Solonker” suture marks the final closural zone in Permian, whereas others insist in middle Paleozoic. Our three study areas, the Hongqi, the Ondor Sum and the Mandula is essential and important to solve those controversies. The litho-tectonic units recognized in the Hongqi-Ondor Sum area include the Hongqi-Ondor Sum mélange belt, the Bainaimiao arc belt, North China Craton and post-orogenic unconformably sedimentary rocks. The Hongqi-Ondor Sum mélange belt experienced two phase ductile deformation and one phase ductile-brittle deformation. D1 is responsible for the regional greenschist foliation S1, elongated mineral lineation L1, and intrafolial fold F1. The kinematic criteria indicates a top-to-the-NW shearing sense. D2 is characterized by various sized of unsymmetrical folds with nearly NE axis corresponding to the NW thrust shearing. D3 formed the regional framework in the Hongqi and the Ondor Sum areas. The Mandula area contains olistostrome sediments, turbiditic sediments and volcano-sedimentary rocks. Detrital zircon grains in sedimentary samples argue the Mandula study area received the southern Bainaimiao arc materials and coeval Permian volcanic erupting materials nearby. The sediments and volcanic rocks in Mandula area subject a nearly NW-SE or N-S compressional shortening. The geological data support that an Early Paleozoic subduction and collsioan, Late Palezoic rifting and rift closure model. The so called “Solonker” ophiolitic fragments indeed are olistostrome. Typical ophiolite components are not observed in the Mandula area.

Le Centre-Est de la Mongolie intérieure, faisant la partie sud-est de la Ceinture Orogénique de l'Asie Centrale (CAOB), est une zone de clé pour étudier l'histoire de l’accrétion-collision entre la Chine du Nord (NCC) et les blocs continentaux du Nord. Les contraintes du cadre tectonique et de la connaissance de l’évolution tectonique sont importantes pour comprendre l’accrétion de la CAOB car il n’y a pas de consensus sur le mode et la période de l'accrétion entre NCC et les blocs du Nord. Par conséquent, des études pluridisciplinaires ont été effectuées sur les roches sédimentaires et magmatiques du Paléozoïque supérieur dans le centre-oriental de la Mongolie Intérieure. Sur la base de nos études sédimentologiques, géochronologiques, géochimiques et paléomagnétiques, et compte tenu des résultats précédents en pétrographie, géochimie et paléontologie, l'évolution sédimentaire et tectonique du Paléozoïque supérieur du Centre-Oriental de la Mongolie Intérieure a été bien établie. Les études détaillées en sédimentologie et géochimie montrent une transition entre les dépôts molassiques du Dévonien à la dénudation du Carbonifère inférieur et les sédiments marins du Carbonifère supérieure vers les dépôts de bassin d'extension au Permien. D’après nos analyses détaillées des faciès sédimentaires, des caractéristiques géochimiques des roches magmatiques et nos données paléomagnétiques, nous proposons un modèle géodynamique de subduction-collision-extension post-orogénique pour le Paléozoïque au Centre-Oriental de la Mongolie Intérieure. / Central-eastern Inner Mongolia, located in the southeastern part of the Central Asian Orogenic Belt (CAOB), is a key area to study the collisional-accretionary history between the North China Craton (NCC) and the northern continental blocks. The establishment of precise constraints of this tectonic framework and evolutional history are important to understand the accretion of CAOB. However, no any consensus has been achieved about the way and the timing of the accretion between NCC and the northern blocks. Therefore, multidisciplinary studies have been carried out on the Late Paleozoic strata and magmatic rocks in central-eastern Inner Mongolia. Based on our sedimentological analyses, detrital zircon geochronological constraints, geochemical studies and paleomagnetic investigations, integrating the previous results in petrology, geochemistry and paleontology, the Late Paleozoic sedimentary-tectonic evolution of the central-eastern Inner Mongolia has been established. Detailed sedimentological and geochemical studies show a transition from the Devonian molassic deposits to the Early Carboniferous denudation and from the Late Carboniferous inland-sea sediments to the Permian extensional basin deposits. According to the comprehensive analyses on sedimentary facies, geochemical characteristics and paleomagnetic data, we propose a Paleozoic subduction-collision- post-orogenic extension tectonic model for central-eastern Inner Mongolia.

Ce mémoire propose une analyse socio-historique d'un cas extrême de changement social par son ampleur et sa rapidité: l'apparition ex-nihilo, à partir des années 1990, d'une population de plus de 100 000 mineurs artisanaux en Mongolie. Pour ce faire, il offre, premièrement, des outils théoriques au lecteur pour comprendre la tension entre permanence et mouvement qui anime les sociétés humaines. Deuxièmement, il identifie les tendances récurrentes de l'histoire mongole pour rendre le présent plus intelligible. Troisièmement, il détaille les principales caractéristiques contemporaines de ce nouveau phénomène, ainsi que ses potentialités pour le proche avenir. Mais surtout, à chaque étape, il construit une théorie locale et partielle du changement social, qui montre l'impact croissant de l'État moderne et de son idéologie du progrès et de la rationalité dans la vie de tous les individus, qui laisse les plus marginaux d'entre eux de plus en plus dépourvus d'influence sur leur environnement. / This paper outlines a socio-historic analysis of an extreme case of social change in Mongolia in the 1990s, which saw the sudden emergence of more than 100 000 artisanal miners. The first chapter discusses the relevant concepts which assist to develop an understanding of the tensions between stability and movement in human societies and how this in turn produces change. The next chapter identifies the recurring trends of Mongolian history and how that contributes to the present situation. The final chapter details the characteristics of this phenomenon and how it might develop in the near future. This paper proposes a new theory that, applied to this specific case, illustrates the impacts of the modern state on each individual and how it diminishes control from the marginalised groups of society.

It is hotly debated about the final closural time and position of the Paleo-Asian Ocean. Some geologists advocated the "Solonker" suture marks the final closural zone in Permian, whereas others insist in middle Paleozoic. Our three study areas, the Hongqi, the Ondor Sum and the Mandula is essential and important to solve those controversies. The litho-tectonic units recognized in the Hongqi-Ondor Sum area include the Hongqi-Ondor Sum mélange belt, the Bainaimiao arc belt, North China Craton and post-orogenic unconformably sedimentary rocks. The Hongqi-Ondor Sum mélange belt experienced two phase ductile deformation and one phase ductile-brittle deformation. D1 is responsible for the regional greenschist foliation S1, elongated mineral lineation L1, and intrafolial fold F1. The kinematic criteria indicates a top-to-the-NW shearing sense. D2 is characterized by various sized of unsymmetrical folds with nearly NE axis corresponding to the NW thrust shearing. D3 formed the regional framework in the Hongqi and the Ondor Sum areas. The Mandula area contains olistostrome sediments, turbiditic sediments and volcano-sedimentary rocks. Detrital zircon grains in sedimentary samples argue the Mandula study area received the southern Bainaimiao arc materials and coeval Permian volcanic erupting materials nearby. The sediments and volcanic rocks in Mandula area subject a nearly NW-SE or N-S compressional shortening. The geological data support that an Early Paleozoic subduction and collsioan, Late Palezoic rifting and rift closure model. The so called "Solonker" ophiolitic fragments indeed are olistostrome. Typical ophiolite components are not observed in the Mandula area.

This study demonstrates the flexible nature of relations between “peripheral” polities imperial “core” polities. The decentralized nature of the Mongol and Iroquois confederacies enabled them to dictate terms during negotiations with the Ming dynasty or British, respectively, giving them a higher degree of agency in their relations. Comparing the experiences of the Mongols and Iroquois provides a better understanding of how indigenous confederacies acted and reacted under similar circumstances. Likewise, this study aims to demonstrate the capacity for “peripheral” confederacies to resist, selectively adapt, and negotiate with “core” empires. / Confederacy in action -- Iroquois historiography -- Mongol historiography -- Social structures and foundation myths -- "Relative" relations. / Department of History

The limnological knowledge of waters in arid regions, especially Mongolia, is still insufficient. It was the goal of the Mongolian-German research project “Limnological Particularities of Characteristic Waterbodies in the Uvs Nuur Basin” to develop a systematic inventory of waters, describe their morphological, hydrophysical, chemical and biological characteristics and to generalize the framework of abiotic and biotic factors that determine their character. During the field work, carried out from 1996 to 1999, samples of water, sediments, benthic and planktonic biota were taken from 76 places at 15 stagnant water bodies, 21 streams and several groundwater bodies; morphological, hydrological, physical and hydrochemical measurements were made. Chemical and biological analyses were carried out in Germany. The most important taxonomical groups were determined by German and international specialists. The results of the work are presented and discussed separately for running waters, lakes and groundwater. Based on these findings, several general topics are dealt with: factors shaping the character of water bodies, food webs, biogeography, spatial sequence of water bodies, typology and protection issues. A checklist of 596 taxa was compiled; 109 additional taxa from the Russian and Mongolian literature were included. Two species (Cyclops glacialis Flößner 2001 and Acanthocorbis mongolica Paul 2011) were new for the science and 103 species were new reports for Mongolia. A regional stream typology with 11 different types was developed using the criteria ecoregion, altitude and catchment area. The typology developed for stagnant waters comprises 9 types based on altitude, lake area, existence of an outflow and relative depth. This dissertation comprises 139 pages and an appendix of 59 pages, 50 tables, 94 figures and a map.

This thesis analyses the democratization process of Mongolia by applying a qualitative, theory consuming and theory developing case study. The study analyses if three national factors: governance, values and civil society can be claimed to be driving forces behind the Mongolian democratization process. The finds are positive in that all three factors are found to have played some part in the forenamed process. Though all factors are claimed to be visible in this study they are not equally so as governance as a factor has been given a much larger role in previous studies of the Mongolia democratization process. The study also tries to discover new factors for democratization, previously not defined as such. One find is claimed in redefining of history and through this an emergence of a new national identity. This redefining of history was caused by the oppositions tries to gain legitimacy but also might be a driving force behind the democratic process. The study also argues that one plausible truth for the emergence of more democratic values and the rise of civil society might lie in the method that the opposition managed to redefine the country’s history and in so doing created a new Mongolian identity.

On observe depuis 2005 une sismicité intense à 10 km d'Oulan Bator ce qui a permis d'identifier une faille active, Emeelt, sur le terrain. Après le calcule d'un modèle de vitesse 3D, j'ai appliqué la tomographie double différence pour obtenir une localisation précise des séismes. Ils marquent au moins trois branches parallèles orientées N147° comme la faille vue en surface. L'activité sur la faille principale d'Emeelt (MEF) s’étend sur 15 km, les branches Ouest et Est, moins actives, sur 10 km. La profondeur de l'activité s'étend entre 4 et 15 km. L'activité sismique semble concentrée à l'intersection avec des failles Mésozoïques et les contrastes Vs/Vs suggèrent la présence de fluides. Les 10 essaims identifiés montrent une activité croissante et une migration spatiale avec le temps. Le calcul de 2 scénarios possibles, un M ~ 6.4 et un M ~ 7, indique un important impact sur la ville d'Oulan Bator, avec une intensité minimum de VIII et localement IX pour M=6.4 et X pour M=7. / We observe since 2005 a high seismic activity at 10 km from Ulaanbaatar that allowed us to identify a new active fault, Emeelt, in the field. After computing a 3D velocity model, I applied Double-Difference tomography to obtain a precise localization of earthquakes. They trace at least three parallel branches oriented N147° like the fault seen at surface. The seismic activity on the Main Emeelt Fault (MEF) is along at least 15 km, on the West and East branches, less active, along 10 km. The depth of the seismicity extends between 4 and 15 km. The activity seems concentrated at the intersection with Mesozoic faults and Vp/Vs contrast suggests the presence of fluids. The 10 swarms identified show an increasing activity and a spatial migration with time. The calculation of 2 possible scenarios, one M ~ 6.4 and one M ~ 7, shows an important impact on Ulaanbaatar, with a minimum intensity of VIII and IX for M=6.4 and X for M=7.