An earthquake is a mechanism of stress release along plate boundaries due to relative motion between the Earth's lithospheric blocks. The period in which stresses are accruing across the plate boundary is known as the interseismic portion of the earthquake cycle. This dissertation focuses on interseismic portion of the earthquake cycle to extract characteristics of fault, shear zone and rock properties. Global Positioning System (GPS) data are used to observe the pattern of deformation across two primarily strike-slip fault systems: the Carrizo Segment of the San Andreas Fault (SAF) and the Eastern California Shear Zone (ECSZ). Two sets of GPS data are processed, analyzed and applied to analytic and numerical models describing the interseismic behavior of the earthquake cycle. The Carrizo segment is mature (i.e., had many earthquakes) and has juxtaposed terrains with varying rock properties laterally across the fault system. Lateral variations in rock properties affect the pattern of deformation around strike-slip faults and affect how surrounding rock deforms and if not considered may bias the interpretation of the faulted system. The Carrizo segment separates Franciscan terrain northeast of the fault from Salinian block to the southwest. GPS data are well fit to a model with a 15-25 km weak zone northeast of the Carrizo segment. The long-term slip rate estimated on the SAF is 34-38 mm/yr, with 2-4 mm/yr accommodated on faults to the west. The viscosity for the combined lower crust/upper mantle is estimated at 2-5x10^19 Pa s. This model is consistent with the distribution of rock type and corresponding laboratory data on their material properties, paleoseismic, seismic and magnetotelluric data. The ECSZ is a young (<10 >Myr) system of strike-slip faults including the Owens Valley - Airport Lake, Panamint Valley - Ash Hill - Hunter Mountain and Death Valley - Furnace Creek fault systems. The ECSZ study concentrates on fault evolution by finding the current position of maximum shear across the shear zone and estimating fault rates. Geologic studies suggest that the Death Valley - Furnace Creek fault system on eastern end of the ECSZ was the primary accommodator of slip early in the ECSZ history. This study suggests that the current locus of shear has shifted westward, and resides in the center of the ECSZ under the Panamint Valley - Ash Hill -Hunter Mountain fault system. The model dependent estimated geodetic rate of the Ash Hill - Panamint Valley -Hunter Mountain fault system (4.91-6.11 mm/yr) is faster than geologic estimates (1.6 - 4 mm/yr). The result is interpreted as a simplification of the ECSZ with time, combined with progressive westward migration of deformation. The best estimate for a combined rate across the shear zone is 10 mm/yr (20% of total Pacific-North America motion). The summation of rates obtained by this study is 49 mm/yr, well within estimates obtained by previous studies using independent techniques.

Systeme von Vorlandbecken repräsentieren bedeutende geologische Archive und dienen dem Verständnis von Rückkopplungen zwischen oberflächennahen und tektonischen Prozessen. Außerdem dokumentieren sie die Entwicklung unmittelbar angrenzender Bergketten. Die sedimentären Abfolgen in Vorlandbecken reflektieren das Gleichgewicht zwischen tektonischer Subsidenz, der Bildung langzeitlichen Akkommodationsraumes und des Sedimenteintrages, welcher wiederum die Wirksamkeit von Erosions- und Massenneuverteilungsprozessen wiederspiegelt. Um die Effekte von Klima und Tektonik in einem solchen System zu erforschen, untersuchte ich die Oligo-Miozänen Sedimente in den Vorlandbecken der südlichen Elburs Bergkette, einem intrakontinentalen Gebirge in Nord-Iran, das im Zuge der Arabisch-Eurasischen Kontinent-Kollision herausgehoben wurde. In dieser Studie der Vorlandbeckensedimente wurden Datierungstechniken angewandt (40Ar/39Ar, (U-Th)/He Thermochronologie und Magnetostratigraphie), die Sedimente und deren Herkunft analysiert und die Tonmineralogie, sowie Sauerstoff- und Kohlenstoffisotope untersucht. Die Ergebnisse zeigen, dass auf einer Zeitskala von 105 bis 106 Jahren eine systematische Korrelation zwischen „coarsening upward“ Zyklen und den sedimentären Akkumulationsraten besteht. Während sukzessiver Überschiebungsphasen werden die durch Hebung der Bergkette bereitgestellten groben Kornfraktionen in proximale Bereiche des Beckens geliefert und feinkörnige Fazies in distalen Beckenregionen abgelagert. Variationen in der Sedimentherkunft in Phasen größerer tektonischer Aktivität zeugen von erosionaler Abdeckung und/oder der Umorganisation natürlicher Entwässerungsstrukturen. Außerdem zeigen die Untersuchungen an stabilen Isotopen, dass die verstärkte tektonische Aktivität das Anwachsen der Topographie förderte und damit die Wirksamkeit einer topographischen Barriere erhöhte. Wenn aufgrund nachlassender Beckenabsenkung die grobe Kornfraktion nicht vollständig im Nahbereich des Beckens aufgenommen werden kann breitet sie sich in ferne Beckenregionen aus. Im Elburs wird die verringerte Subsidenz durch eine interne Hebung des Vorlandes hervorgerufen und ist mit einer lateralen Stapelung von Flussbetten assoziiert. Dokumentiert wird dies anhand konsequenten Schichtwachstums, tektonischer Schrägstellung und sedimentärer Umlagerung. Gleichzeitig nehmen die Sedimentationsraten zu. Die Sauerstoff-Isotope der Paläoböden zeigen, dass dieser Anstieg mit einer Phase feuchteren Klimas einhergeht, wodurch Oberflächenprozesse effizienter werden und Heraushebungssraten steigen, was eine positive Rückkopplung erzeugt. Des Weiteren zeigen die isotopischen und sedimentären Daten, dass seit 10-9 Millionen Jahren (Ma) das Klima durch saisonalen Anstieg der Niederschläge zunehmend feuchter wurde. Da bedeutende klimatische Veränderungen zu dieser Zeit auch im Mittelmeerraum und Asien beobachtet wurden, ist anzunehmen, dass die klimatische Veränderung, die im Elburs Gebirge beobachtet wird, höchstwahrscheinlich Änderungen der atmosphärischen Zirkulationen der nördlichen Hemisphäre reflektiert. Aus den Ergebnissen dieser Studie lassen sich zusätzliche Implikationen für die Entwicklung des Elburs Gebirges und die Arabisch-Eurasische kontinentale Kollisionszone ableiten. Die orogen-weite Hauptdeformation propagierte nicht gleichmäßig nach Süden, sondern seit dem Oligozän schrittweise vorwärts und rückwärts. Insbesondere von ~17,5 bis 6,2 Ma wurde das Gebirge durch eine Kombination aus frontaler Akkretion und interner Keildeformation in Schritten von 0,7 bis 2 Millionen Jahren herausgehoben. Darüber hinaus deuten die Sedimentherkunftsdaten darauf hin, dass sich noch vor 10-9 Ma die Haupteinengungsrichtung von NW-SE nach NNE-SSW veränderte. Regional erlaubt die Geschichte der untersuchten Becken und angrenzenden Gebirgszüge Rückschlüsse auf ein neues geodynamisches Model zur Entwicklung der Arabisch-Eurasischen kontinentalen Kollisionszone. Zahlreiche Sedimentbecken des Elburs Gebirges und anderer Lokalitäten der Arabisch-Eurasischen Deformationszone belegen einen Wechsel von einem tensionalen zu einem kompressionalen tektonischen Regime vor ~36 Ma . Dieser Wechsel könnte den Beginn der Subduktion von gedehnter arabischer kontinentaler Lithosphäre unter Zentral-Iran bedeuten, was zu einer moderaten Plattenkopplung und Deformation von Unter- sowie Oberplatte geführt hat. Der Anstieg der Deformationsraten im südlichen Elburs Gebirge seit ~17,5 Ma lässt vermuten, dass die Oberplatte, wahrscheinlich aufgrund steigender Plattenkopplung, seit dem frühen Miozän signifikant deformiert wurde. Diese Veränderung könnte der Subduktion mächtigerer arabischer kontinentaler Lithosphäre zugeschrieben werden und den Anfang echter kontinentaler Kollision bedeuten. Dieses Model erklärt daher die Zeitverzögerung zwischen der Initiation der Arabisch-Eurasischen kontinentalen Kollision (Eozän-Oligozän) and dem Beginn ausgedehnter Deformation in der Kollisionszone (Miozän). / Foreland-basin systems are excellent archives to decipher the feedbacks between surface and tectonic processes in orogens. The sedimentary architecture of a foreland-basin system reflects the balance between tectonic subsidence causing long-term accommodation space and sediment influx corresponding to efficiency of erosion and mass-redistribution processes. In order to explore the effects of climatic and tectonic forcing in such a system, I investigated the Oligo-Miocene foreland-basin sediments of the southern Alborz mountains, an intracontinental orogen in northern Iran, related to the Arabia-Eurasia continental collision. This work includes absolute dating methods such as 40Ar/39Ar and zircon (U-Th)/He thermochronology, magnetostratigraphy, sedimentological analysis, sandstone and conglomerate provenance study, carbon and oxygen isotope analysis, and clay mineralogy study. Results show a systematic correlation between coarsening-upward cycles and sediment accumulation rates in the basin on 105 to 106yr time scales. During thrust loading phases, the coarse-grained fraction supplied by the uplifting range is stored in the proximal part of the basin (sedimentary facies retrogradation), while fine-grained sediments are deposited in distal sectors. Variations in sediment provenance during these phases of enhanced tectonic activity give evidence for erosional unroofing phases and/or drainage-reorganization events. In addition, enhanced tectonic activity promoted the growth of topography and associated orographic barrier effects, as demonstrated by sedimentologic indicators and the analysis of stable C and O isotopes from calcareous paleosols and lacustrine/palustrine samples. Extensive progradation of coarse-grained deposits occurs during phases of decreased subsidence, when the coarse-grained fraction supplied by the uplifting range cannot be completely stored in the proximal part of the basin. In this environment, a reduction in basin subsidence is associated with laterally stacked fluvial channel deposits, and is related to intra-foreland uplift, as documented by growth strata, tectonic tilting, and sediment reworking. Increase in sediment accumulation rate associated with progradation of vertically-stacked coarse-grained fluvial channels also occurs. Paleosol O-isotope data shows that this increase is related to wetter climatic phases, suggesting that surface processes are more efficient and exhumation rates increase, giving rise to a positive feedback. Furthermore, isotopic and sedimentologic data show that starting from 10-9 Ma, climate became less arid with an increase in seasonality of precipitation. Because important changes were also recorded in the Mediterranean Sea and Asia at that time, the evidence for climatic variability observed in the Alborz mountains most likely reflects changes in Northern Hemisphere atmospheric circulation patterns. This study has additional implications for the evolution of the Alborz mountains and the Arabia-Eurasia continental collision zone. At the orogenic scale, the locus of deformation did not move steadily southward, but stepped forward and backward since Oligocene time. In particular, from ~ 17.5 to 6.2 Ma the orogen grew by a combination of frontal accretion and wedge-internal deformation on time scales of ca. 0.7 to 2 m.y. Moreover, the provenance data suggest that prior to 10-9 Ma the shortening direction changed from NW-SE to NNE-SSW, in agreement with structural data. On the scale of the entire collision zone, the evolution of the studied basins and adjacent mountain ranges suggests a new geodynamic model for the evolution of the Arabia-Eurasia continental collision zone. Numerous sedimentary basins in the Alborz mountains and in other locations of the Arabia-Eurasia collision zone record a change from a tensional (transtensional) to a compressional (transpressional) tectonic setting by ~ 36 Ma. I interpret this to reflect the onset of subduction of the stretched Arabian continental lithosphere beneath central Iran, leading to moderate plate coupling and lower- and upper-plate deformation (soft continental collision). The increase in deformation rates in the southern Alborz mountains from ~ 17.5 Ma suggests that significant upper-plate deformation must have started by the early Miocene most likely in response to an increase in degree of plate coupling. I suggest that this was related to the subduction of thicker Arabian continental lithosphere and the consequent onset of hard continental collision. This model reconciles the apparent lag time of 15-20 m.y between the late Eocene to early Oligocene age for the initial Arabia-Eurasia continental collision and the onset of widespread deformation across the collision zone to the north in early to late Miocene time.

The aquatic plant Ipomoea aquatica is a popular vegetable in Southeast Asia, often cultivated in nutrient rich and polluted waters. The overall aim of this thesis was to estimate potential risks for human health and reduced plant growth due to accumulation and toxicity of total-Hg, methyl-Hg, Cd and Pb. In plants from cultivations in Thailand, the concentrations of Cd and Pb in the shoots were well beneath recommended maximum values for human consumption, but at some sites the Hg concentrations were high. It was demonstrated that I. aquatica has the capacity to accumulate much higher Cd and Pb concentrations in the shoots than found in field-cultivations, before exhibiting toxic symptoms. The Hg concentrations, however, occasionally reached levels that are toxic for the plant. Up to11% of total-Hg was methyl-Hg, the most toxic Hg species, though at one site it was 50-100%. To study if methyl-Hg is formed in I. aquatica, plants were exposed to inorganic Hg through the roots. Of the Hg that reached the young, metabolically active parts of the shoots, a part was transformed to methyl-Hg. A major proportion of absorbed metals was retained in the roots, which had a high tolerance for high internal metal concentrations. The nutrient level did influence accumulation and effects of Hg, Cd and Pb in I. aquatica. Low external nutrient levels resulted in increased metal accumulation in the shoots and in metal-induced toxic effects in the plant at low external metal levels. A generous supply of sulphur or nitrogen induced formation of thiol-rich peptides in I. aquatica, compounds that have a metal detoxifying effect in plants. To conclude, the levels of Cd and Pb in field cultivated I. aquatica do not pose any apparent threat to human health or risk for reduced plant growth. The levels of Hg however, were high at some sites and could be a health threat, for children and foetuses in particular, and especially considering the presence of methyl-Hg. The use of fertilizers is favourable as it reduces the risk for increased metal concentrations in I. aquatica and for reduced crop yields.

To date, remote sensing estimates of snow water equivalent (SWE) in mountainous areas are very uncertain. To test passive microwave algorithm estimations of SWE, a validation data set must exist for a broad geographic area. This study aims to build a data set through field measurements and statistical techniques, as part of the Canadian IPY observations theme to help develop an improved algorithm. Field measurements are performed at, GIS based, pre-selected sites in the Central Yukon. At each location a transect was taken, with sites measuring snow depth (SD), density, and structure. A mixed effects multiple regression was chosen to analyze and then predict these field measurements over the study area. This modelling strategy is best capable of handling the hierarchical structure of the field campaign. A regression model was developed to predict SD from elevation derived variables, and transformed Landsat data. The final model is: SD = horizontal curvature + cos( aspect) + log10(elevation range, 270m) + tassel cap: greenness, brightness (from Landsat imagery) + interaction of elevation and landcover.This model is used to predict over the study area. A second, simpler regression links SD with density giving the desired SWE measurements. The Root Mean Squared Error (RMSE) of this SD estimation is 25 cm over a domain of 200 x 200 km. This instantaneous end of season, peak accumulation, snow map will enable the vali- dation of satellite remote sensing observations, such as passive microwave (AMSR-E), in a generally inaccessible area.

To date, remote sensing estimates of snow water equivalent (SWE) in mountainous areas are very uncertain. To test passive microwave algorithm estimations of SWE, a validation data set must exist for a broad geographic area. This study aims to build a data set through field measurements and statistical techniques, as part of the Canadian IPY observations theme to help develop an improved algorithm. Field measurements are performed at, GIS based, pre-selected sites in the Central Yukon. At each location a transect was taken, with sites measuring snow depth (SD), density, and structure. A mixed effects multiple regression was chosen to analyze and then predict these field measurements over the study area. This modelling strategy is best capable of handling the hierarchical structure of the field campaign. A regression model was developed to predict SD from elevation derived variables, and transformed Landsat data. The final model is: SD = horizontal curvature + cos( aspect) + log10(elevation range, 270m) + tassel cap: greenness, brightness (from Landsat imagery) + interaction of elevation and landcover.This model is used to predict over the study area. A second, simpler regression links SD with density giving the desired SWE measurements. The Root Mean Squared Error (RMSE) of this SD estimation is 25 cm over a domain of 200 x 200 km. This instantaneous end of season, peak accumulation, snow map will enable the vali- dation of satellite remote sensing observations, such as passive microwave (AMSR-E), in a generally inaccessible area.

In the last thirty years, capitalist social relation on the one hand, created a world that is interconnected in the means of economic and political / on the other hand, produced differentiated and fragmented uneven spaces. In this context, social theory has interested in space and spatial differences, and inserted space into analysis of social relations for some time. In this thesis, the current issue of the construction of subnational regional space is explored through a conceptual approach in which space is included in social theory. Methodologically, a non-dualistic social analysis is considered and the notion of space is attempted to incorporate into this analysis. In this extent, David Harvey&rsquo / s historical-geographical approach, Dick Bryan&rsquo / s identification of capital fractions with different spatial forms of circuit of capital within the capital accumulation process and Jamie Gough&rsquo / s considerations of economic and political relations with scalar aspects are used. The thesis evaluated the law on the Regional Development Agencies and arguments on regional development and regional governance as the process of construction of subnational regional space, and examined the struggle for setting up of Regional Development Agencies within Turkish state. In this framework, thesis came to the conclusion that the changes in the scale of social relations is associated with changes in power relations among social agents, developed through class struggle, and articulated by political projects

This thesis aims to discuss the argument of exhaustion of economic globalization as an American foreign policy principle. This study argues that economic globalization is intended to restore declining American hegemony started in 1970s, but it has eventually given way to the argument of &ldquo / return of the geopolitics&rdquo / . The return of the geopolitics is an imperial, expansionist drive as a new foreign policy imperative for United States. The new developments in the international arena in the post-cold war era and especially after the September 11, 2001 brought the end of the globalization as an American project. Globalization is replaced with geopolitics in the transition period from hegemony to empire in United States foreign policy. Because there are new threats for United States in the twenty-first century such as the rise of new global actors in world politics or international competition for oil resources in the strategic regions of the world. In this framework, this study focuses on the rise of new, alternative &ldquo / great powers&rdquo / (European Union, China etc...).

Under capitalist mode of production urban processes gain specific features and meanings. Fundamental is the relationship between processes of capital accumulation and the production of built environment. In this context, the capital switching theory claims that as profit levels are lowered, the probability that higher levels of capital tending to enter the property sector increases. In the first stage of a two-staged research, a macro-analysis on construction activities in Turkey limited to post-1980 period indicates that there no counter-cyclical relationship prevails between productive sectors of the economy and construction activities. It is observed that the state intervention and its supportive policies regarding the production of built environment are the dominant determinants in the Turkish case. Based on these findings, a second focus was on the relationships between the state and capital engaged in the production of urban built environment. Various forms of state intervention, mostly as examples of deregulation and liberalization of planning controls and urban development legislation are identified at this stage. The major findings lead to the conclusion that urban processes are open to the profit-oriented and speculative efforts of political actors as well as the economic actors. Hence the necessity of development of counter-strategies and policies as parts of planning and urban development system verified.

Oil loss mechanisms in internal combustion engines have been subject to many researches. By the help of technological developments effects of several problems due to oil losses were examined and tried to be reduced. Environmental pollution and performance loss are important issues that oil consumption in internal combustion engines contribute. In this study the effects of individual parameters on the oil accumulation in 2nd land crevice of internal combustion engines, volume between top compression rings, were investigated. The study aimed to investigate the effects of oil film thickness and oil film temperature on the oil accumulation in the 2nd land which contributes to one of the mechanisms of oil consumption in internal combustion engines. Controlled experiments were performed on a modeled piston cylinder assembly. It was seen that oil accumulated in the 2nd land crevice by blow-by gases was affected by the film thickness of lubricating oil and the temperature of the lubricating oil. The amount of oil accumulated increased with increasing oil film thickness. The results also showed that below oil film thickness of 45 &amp / #956 / m / amount of oil accumulated increased with the increase of oil temperature.

ABSTRACT During Dutch Colonial domination, one of the most controversial themes was that why the Indonesian society had failed to generate an indigenous bourgeoisie. Since the post-colonial era, most developing countries are facing three dilemmas: the state building, the formation of social classes, the capital accumulation. For the methodology, the dissertation both takes a¡§state-center¡¨view and tries to apply an approach to explore the formation of Bureaucratic Capitalist during Suharto time with a view of historical-structure from the concept of state, class and capital. Furthermore, the studies will focus on three fields. First, why over 350 years, the mercantile policy of the colonial regime had failed to penetrate into the whole Indonesia shaping an indigenous bourgeoisie. Secondly, from 1950 to 1965, President Sukarno had taken the state-capitalism as a developmental strategy why Indonesian society still had not found indigenous bourgeoisie strong enough to take responsibility of leading capitalist revolution. Thirdly, after 1965, in the power of Suharto, the state has played a decisive role in the shaping the development of big entrepreneurs in the post-colonial Indonesia. In addition, the studies will review and provide a critical analysis of the works of Indonesia Studies in the West, and continues to dialogue with the contemporary academician in the field. Key Words: Agricultural Involution, Asian Mode of Production, Pre-capitalism, Dual Economy, Articulation Theory, State Apparatus, Capital Accumulation, Commercialization, Bureaucratic-Capitalist Class