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281.
Steven M. Reddy Graham J. Potts Simon P. Kelley 《Contributions to Mineralogy and Petrology》2001,141(2):186-200
Detailed field and microstructural studies have been combined with high spatial resolution ultraviolet laser 40Ar/39Ar dating of naturally deformed K-feldspar to investigate the direct relationship between deformation-related microstructure and Ar isotope systematics. The sample studied is a ~1,000 Ma Torridonian arkose from Skye, Scotland, that contains detrital feldspars previously metamorphosed at amphibolite-facies conditions ~1,700 Ma. The sample was subsequently deformed ~430 Ma ago during Caledonian orogenesis. The form and distribution of deformation-induced microstructures within three different feldspar clasts has been mapped using atomic number contrast and orientation contrast imaging, at a range of scales, to identify intragrain variations in composition and lattice orientation. These variations have been related to thin section and regional structural data to provide a well-constrained deformation history for the feldspar clasts. One hundred and forty-three in-situ 40Ar/39Ar analyses measured using ultraviolet laser ablation record a range of apparent ages (317-1030 Ma). The K-feldspar showing the least strain records the greatest range of apparent ages from 420-1,030 Ma, with the oldest apparent ages being found close to the centre of the feldspar away from fractures and the detrital grain boundary. The most deformed K-feldspar yields the youngest apparent ages (317-453 Ma) but there is no spatial relationship between apparent age and the detrital grain boundary. Within this feldspar, the oldest apparent ages are recorded from orientation domain boundaries and fracture surfaces where an excess or trapped 40Ar component resides. Orientation contrast images at a similar scale to the Ar analyses illustrate a significant deformation-related microstructural difference between the feldspars and we conclude that deformation plays a significant role in controlling Ar systematics of feldspars at both the inter- and intragrain scales even at relatively low 'bulk' strains. The data show that Ar loss and trapping within the deformed K-feldspars reflects the presence of a deformation-induced population of small diffusion domains in combination with 'short-circuit' diffusion along deformation-induced defects. The complex history of microstructures induced in the K-feldspars during their cooling, alteration, erosion and sedimentation do not appear to be as significant as deformation-induced microstructures in controlling the distribution of apparent ages at the grain scale. 相似文献
282.
Andrew J Dougill Chasca Twyman David S G Thomas & Deborah Sporton 《The Geographical journal》2002,168(3):195-210
Soil degradation assessments for mixed farming systems of the Molopo Basin (North West Province, South Africa and Southern District, Botswana) are provided from farmer–based research, designed to quantify nutrient fluxes across the farming system and to analyze the social, economic, political and environmental factors affecting nutrient management practices. This paper discusses the practical difficulties of how to use participatory farmer–led studies to assess soil degradation extent and its causes, and of then disseminating this information to farming communities and policymakers. Nutrient balance studies show that land degradation is evident on arable fields as soil nutrient depletion (the main threat to poorer manure–reliant farmers) and soil acidification (the main threat to wealthier farmers who have become dependent on inorganic fertilizer additions). Integrated nutrient management strategies involving both compound fertilizer additions and regular manure inputs can mitigate most soil degradation even on the sandy infertile Kalahari soils, but remain infrequently practised. The need to retain nutrient flows through the livestock sector from rangeland to arable land is thus vital to environmental sustainability and offers an applicable entry point for agricultural development initiatives and support. Factors identified as threatening the flow of nutrients from rangelands to arable lands include policy settings in terms of the different support programmes offered to communal farmers, village–level extension advice, household poverty levels and labour constraints. 相似文献
283.
284.
The SWAN model used to study wave evolution in a flume 总被引:1,自引:0,他引:1
Deborah J. Wood Research Assistant Markus Muttray Research Engineer Professor Hocine Oumeraci 《Ocean Engineering》2001,28(7)
The SWAN numerical model is used to model the evolution of JONSWAP wave spectra and hence the significant wave height of waves in a tank. Comparison with experiment has shown that modelling triad interactions in the numerical model leads to too low predictions of spectra and significant wave height and should therefore be excluded. The modelling of the breaking constant was also investigated, by looking at the use of a constant breaking constant, Nelson formula, and Goda formula (added into SWAN for this study). Using a constant value of 0.78 within SWAN gave the best comparison between theory and experiment. 相似文献
285.
Bemis Karen G. Rona Peter A. Jackson Darrell Jones Christopher Silver Deborah Mitsuzawa Kyohiko 《Marine Geophysical Researches》2002,23(2):81-96
Quantitative visualization of acoustic images is used to compare the properties and behavior of high temperature hydrothermal plumes at two sites with different source configurations, increasing our understanding of how plume behavior reflects source configuration. Acoustic imaging experiments were conducted at the Clam Acres area of the Southwest Vent Field, 21°N East Pacific Rise and at Monolith Vent, North Cleft segment, Juan de Fuca Ridge. At Clam Acres, black smokers discharge from two adjacent chimneys which act as point sources, whereas multiple vents at Monolith Vent define a distributed elliptical source. Both plumes exhibit consistent dilution patterns, reasonable fits to the expected power law increase in centerline dilution with height, and simple bending of plume centerlines in response to ambient currents. Our data suggest that point source vents are associated with ordered plume structure, normal entrainment rates, and initial expansion of isosurfaces while distributed source vents are associated with disorganized plume structure, variable entrainment rates, and initial contraction of isosurfaces. 相似文献
286.
Peter J. Treloar Graham J. Potts John Wheeler David C. Rex 《International Journal of Earth Sciences》1991,80(2):411-428
The Nanga Parbat syntaxis, in the NW Himalaya, is a still growing crustal-scale north-trending antiformal structure in the core of which Indian Plate gneisses have been uplifted from beneath the overthrust rocks of the Kohistan island arc. Isotopic and fission track geochronology show that uplift rates within the syntaxis have increased to present day rates of > 6 mm/yr. Uplift has been accommodated by a combination of initial northwest verging thrusting on the western margin of the syntaxis, followed by crustal scale folding within the syntaxis and latterly by dextral reverse faulting on the western margin. This thrusting, folding and faulting is the effect of deformation at the north-western lateral tips of the main Himalayan thrusts where they interfere with the south-southeast verging thrusts of the northwest Himalaya.
Zusammenfassung Nanga Parbat Konvergenz im nordwestlichen Himalaya ist eine noch im Wachsen begriffene nach Norden streichende antiformale Struktur im Krustenmaßstab. In ihrem Inneren wurden Gneisse der Indischen Platte aus der Nähe der überschobenen Gesteine des Kohistan Inselbogens herausgehoben. Isotopen- und Spaltspurengeochronologie zeigen, daß das Heraushebungsmaß innerhalb der Konvergenz zu der heutigen Rate von > 6 mm/a angestiegen ist. Die Heraushebung hat sich angepaßt an die Kombination von initialer NW-vergenter Überschiebung auf den westlichen Konvergenzrand, die gefolgt wurde von einer krustalen Faltung und lateral von dextraler antithetischer Verwerfung des westlichen Randes. Diese Deckenüberschiebung, Faltung und Verwerfung ist das Resultat der Deformation des nordwestlichen Ausstriches der Himalaya-Hauptüberschiebung, wo sie in Wechselwirkung mit der SSE-vergenten Überschiebung des NW-Himalayas steht.
Résumé La convergence du Nanga Parbat, dans le nordouest de l'Himalaya, est une structure antiforme d'orientation nord-sud, d'échelle crustale et toujours active; son cur est occupé par des gneiss de la plaque indienne qui ont été soulevés à travers les roches charriées de l'arc insulaire du Kohistan. Les données géochronologiques obtenues à partir des isotopes et des traces de fission montrent que le taux de soulèvement a augmenté dans cette structure jusqu'à la valeur actuelle de plus de 6 mm/an. Le soulèvement s'est effectué par la combinaison d'un charriage initial, à vergence nordouest, sur la bordure ouest de la convergence, suivi d'un plissement d'échelle crustale dans la convergence et, latéralement, d'une fracturation par faille dextre inverse sur sa bordure ouest. Ce charriage, ce plissement et cette fracturation sont l'expression de la déformation à l'extrémité latérale nord-ouest des charriages principaux de l'Himalaya, où ils interfèrent avec les charriages à vergence sud- sud-est de l'Himalaya septentrional.
. , , , . , , , , , .. 6 /. , NW, , , . , , SSE .相似文献
287.
288.
Agricultural tourism incorporates visits to farms for the purposes of on‐site retail purchases, enjoyment, and education. Long popular in the European Union (EU), agritourism is gaining popularity throughout the United States. Interest has grown as a result of stagnant grain prices, rising farm costs, and growing international competition. For rural areas seeking new economic options, the potential of these operations to generate new sources of income through sales and horizontal linkages to other tourism‐based activities has sparked interest beyond the farm gate. This article, based on a survey and a statistical analysis of 300 agritourism operations in Michigan, summarizes factors associated with successful operations. 相似文献
289.
Deborah Thien 《Area》2005,37(4):450-454
290.
This paper investigates the ways in which national and regional policies relate to farming activities and concerns amongst the rural population in an area of southern Africa. The struggle to make a living through farming was a common theme to emerge from research about changing livelihoods in response to both variability in the environment and changes in policy. This local discourse echoed regional debates about land and agrarian reform in post-apartheid South Africa and the uncertain future of mixed farming in Botswana. It also raised broader questions about the viability of the future of small-medium-scale farming systems in rural areas in Africa, especially those within dynamic dryland environments such as the Kalahari. This paper looks specifically at the links between poverty and asset holding and aims to identify the ways in which people are or are not able to utilise or mobilise these assets in times of need. We argue that this can vary significantly between seemingly similar settlements, and similar households and that understanding this complexity is the key to recognising how future interventions many impact upon people’s lives. Too often, in the quest to produce understandings of poverty and livelihoods, the complexity, incongruity and reality of day-to-day practices are overlooked. Thus we seek to draw out the interactions between policy and natural resource use, and the capital asset changes involved in these interactions, which influence the sustainability of livelihoods and the differing levels of poverty and vulnerability. 相似文献