Добірка наукової літератури з теми "Geology Australia Fleurieu Peninsula (S.A.)"

RESUMENLa presente investigación ahonda en el tratamiento integral de fuentes geohistóricas textuales. Está basada en la recuperación, el análisis y la apertura de nuevas fórmulas de conocimiento científico abiertas y extensivas a la sociedad global. Entre 1850 y 1940 se elaboran en España más de cuatrocientas obras médicas (geografías o topografías médicas), bajo influencia de las teorías higienistas en el urbanismo y la sociedad en su conjunto, que constituyen unas fuentes de información y documentación enormemente valiosas, y relativamente poco estudiadas, para el conocimiento de los espacios, urbanos y rurales, de la época. El uso del método hipotético-deductivo, modelo de amplia utilización en las ciencias geográficas y las humanidades, ha establecido como hipótesis fundamental que el paisaje y el territorio, y la información contenida en las obras médico-geográficas “Datos médico-topográficos de Ciudad Rodrigo” (1899) y “Datos para la geografía médica de Ciudad Rodrigo” (1920), se utilizarán como base para el análisis de la información que, a escala geográfica, aporta esta tipología documental, estableciendo una metodología para la extracción de información geográfica contenida en documentación histórica. Con ello, se pretende optimizar el uso de fuentes secundarias de conocimiento sobre el territorio y la sociedad, teniendo en cuenta la variedad y cantidad de información que se puede extraer de ellos, abriendo, a la vez, una vía de investigación que liga la salubridad del territorio y las estrategias para abordar problemas territoriales desde la geografía humana e histórica. Palabras clave: fuentes geohistóricas, topografías médicas, higienismo urbano, naturalismo terapéuticoTopónimos: Ciudad Rodrigo (Salamanca)Periodo: siglos xix y xx ABSTRACT This research delves into the comprehensive treatment of textual geohistorical sources based on the recovery, analysis and opening of new formulas of scientific knowledge open and extensive to global society. Between 1850 and 1940, more than four hundred medical works (medical geographies or topographies) were produced in Spain under the influence of hygienist theories in urban planning and constituting society a source of valuable information and documentation relatively little studied for the knowledge of the urban and rural spaces of the time. The use of the hypothetical-deductive method, a model widely used in geographical sciences and humanities, has established as a fundamental hypothesis that landscape and the territory and the information contained in the Medical-geographical works “Medical-topographical Data of Ciudad Rodrigo” (1899) and “Data for the Medical Geography of Ciudad Rodrigo” (1920), will be used as a basis for the analysis of the information that, on a geographical scale, provides this documentary typology and proposes a methodology for the extraction of geographic information contained in historical documentation. With this, it is intended to optimize the use of secondary sources of knowledge about the territory and society considering the variety and amount of information that can be extracted from them and opening, at the same time, a path of research that links health of the territory and the strategies to the approach territorial problems from the human and historical geography. Keywords: geohistorical sources, medical topographies, urban hygiene, therapeutic naturalismPlace names: Ciudad Rodrigo (Salamanca)Period: 19th and 20th centuries REFERENCIASArroyo Ilera, F. y Camarero Bullón, C., “Water for Madrid: The Problems of Water Supply in a Pre-industrial Capital”, en The History of Water Management in the Iberian Peninsula. Trends in the History of Science. Berlin, Birkhäuser, Cham, 2019, pp. 67- 88.Beattie, J. “Imperial landscapes of health: Place, plants and people between India and Australia, 1800´s‐1900´s”, Health and History, 14-1, (2012), pp. 100-120.Brügelmann, J. “Observations on the Process of Medicalization in Germany, 1770-1830, Based on Medical Topographies”, Réflexions historiques, 9 (1-2) (1982), pp. 131-149.Cárdenes, V., Ponce de León, M., Rodríguez, X. 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Ciudad Rodrigo: Imp. de la Vda. e Hijos de Cuadrado, 1899, 102 pp. Oosterom, J. “The importance of hygiene in modern society”, International Biodeterioration Biodegradation, Volume 41, Issues 3–4, (1998), pp. 185-189.Parr, H. “Medical geography: critical medical and health geography?”, Progress in Human Geography, 22-2, (2004), pp. 246-257.Piovan S.E. “The Geohistorical Approach in Environmental and Territorial Studies”, en The Geohistorical Approach. Berlin, Springer Geography, 2020, pp. 5-37. Porras Galló, M. I. “Luchando contra una de las causas de invalidez: antecedentes, contexto sanitario, gestación y aplicación del decreto de vacunación obligatoria contra la viruela de 1903”. Asclepio, vol. LVI-1 (2004), pp. 145- 168.Prats, L. “La Catalunya rància les condicions de vida materials de les classes populars a la Catalunya de la Restauració segons les topografies mèdiques”. Barcelona, Ed. Alta Fulla, 1996.Sánchez Manzano, M., “Datos para la geografía médica de Ciudad Rodrigo”. 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The antiquity of the Australian landscape has long been the subject of debate, with some studies inferring extraordinary longevity (>108 myr) for some subaerial landforms dating back to the early Paleozoic. A number of early Permian glacial erosion surfaces in the Fleurieu Peninsula, southeastern Australia, provide an opportunity to test the notion of long-term subaerial emergence, and thus tectonic and geomorphic stability, of parts of the Australian continent. Here we present results of apatite fission track analysis (AFTA) applied to a suite of samples collected from localities where glacial erosion features of early Permian age are developed. Our synthesis of AFTA results with geological data reveals four cooling episodes (C1-4), which are interpreted to represent distinct stages of exhumation. These episodes occurred during the Ediacaran to Ordovician (C1), mid-Carboniferous (C2), Permian to mid-Triassic (C3) and Eocene to Oligocene (C4).The interpretation of AFTA results indicates that the Neoproterozoic−Lower Paleozoic metasedimentary rocks and granitic intrusions upon which the glacial rock surfaces generally occur were exhumed to the surface by the latest Carboniferous−earliest Permian during episodes C2 and/or C3, possibly as a far-field response to the intraplate Alice Springs Orogeny. The resulting landscapes were sculpted by glacial erosive processes. Our interpretation of AFTA results suggests that the erosion surfaces and overlying Permian sedimentary rocks were subsequently heated to between c. 60 and 80°C, which we interpret as recording burial by a sedimentary cover comprising Permian and younger strata, roughly 1 km in thickness. This interpretation is consistent with existing thermochronological datasets from this region, and also with palynological and geochronological datasets from sediments in offshore Mesozoic−Cenozoic-age basins along the southern Australian margin that indicate substantial recycling of Permian−Cretaceous sediments. We propose that the exhumation which led to the contemporary exposure of the glacial erosion features began during the Eocene to Oligocene (episode C4), during the initial stages of intraplate deformation that has shaped the Mt Lofty and Flinders Ranges in South Australia. Our findings are consistent with several recent studies, which suggest that burial and exhumation have played a key role in the preservation and contemporary re-exposure of Gondwanan geomorphic features in the Australian landscape.

Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1996.
National Grid reference (SI-54)6527 - II, (SI-54) 6627 - III 1:10 000 sheet. Includes bibliographical references (leaves 32-39).

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Whilst the geology of the Rapid Bay-Second Valley area is known to be both structurally and stratigraphically complex, previous workers (Daily, 1963; Evans 1987; Drayton, 1963; Campana and Wilson, 1955) have been unable to agree on many aspects of the area. Neoproterozoic and Cambrian aged sediments were first deposited in an extensional basin, which was formed due to lithospheric thinning, and associated subsidence (Jenkins, 1986, 1990). These rocks have then been subjected to at least one phase of deformation, the Cambro-Ordovician Delamerian Orogeny (Offler & Fleming, 1968; Thompson, 1970). Listric extensional faults were formed both before and during sedimentation of the rocks, which has created narrow zones of weakness that the subsequent compressional event has exploited, creating thrust faults (Flottman et al., 1994). Structural mapping of the area has revealed that it is transected by two thrust faults and is intensely folded in places. Structural data has been collected during eight weeks of field work and has been compiled into a 1:10 000-scale geological map which accurately represents the area. A computer-generated three-dimensional model has been created for the area, based on this map, and cross and profile sections constructed from the data collected. The model was constructed using Vulcan™ software. Strain analysis has also been conducted on many of the folds in the area.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1995

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The study area is located within the Yankalilla-Myponga Proterozoic lnlier, approximately 60km south of Adelaide. The basement rocks are comprised of a mixture of metasediments and intrusives. The metasediments predominantly comprise of quartz-biotite gneisses and schists. They are intruded by basic dykes, pegmatites and an aplite/microgranite. The basic dykes have oceanic basalt affinities and could originally have been formed during an 'aborted rifting' event, but the more felsic rocks are more likely to lie within plate granites. The origin of the 'Houghton' granulite is difficult to ascertain, because it has a varied internal composition and is closely comparable to a diorite and a shale. The basement inlier rocks are found within the overlying unconformable upper Proterozoic Adelaidean System. They have undergone at least four phases of deformation and metamorphism. Mineral assemblages found in the rocks indicate metamorphism reached at least upper amphibolite facies. The maximum pressure and temperature conditions were calculated from microprobe data. They range from 8-10 kb at 550 -650 C. U-Pb isochron dating was performed on the aplite/microgranite of the area and was found to be 1578+\-22Ma ,which places a minimum age on the inlier rocks. This date obtained and the deformation processes recognized are comparable to other basement rocks in South Australia; noticeably the Gaw1er Craton and the Olary Province. This may indicate a homogeneous terrain once spanned most of South Australia during the lower Proterozoic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1988

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A N-E striking elongate aeromagnetic anomaly is observed over the Talisker Mine area, on the southern Fleurieu Peninsula, which has character and amplitude similar to an anomaly observed at Delamere (several kilometres to the north) found to be caused by magnetic Brachina Formation. Geological and geophysical techniques have been used to determine if the rock type at Talisker is also magnetic Brachina Formation, why there is a gap between the two anomalies, and why the anomaly at Talisker ends near the south coast. Geological mapping, microscopy and petrologic studies have been used in conjunction with local ground magnetic surveys and modelling procedures, to reveal magnetic Brachina Formation as the cause of the anomaly at Talisker. Mapping has shown the anomaly to be the result of a sliver of magnetic Brachina Formation caught up within a local zone of intense deformation that extends for at least 1500m across strike, and which outcrops on the coast. The Brachina Formation is sheared out against Cambrian Backstairs Passage Formation to the south, forming the southern end to the anomaly. To the north, the Brachina Formation suffered deeper erosion during Permian times, and is covered by a greater thickness of non-magnetic cover which causes the apparent gap in the aeromagnetic anomaly.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1989