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Titlebook: Methodisches Gestalten und systematisches Entwickeln am Beispiel zukünftiger Fassadenlösungen; Fabian C. Schmid Book 2015 Springer Fachmed

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Fazit und Ausblick,den. Aus dieser Kombination wurde das Niveau der Funktionsintegration als Indiz zu systematischen Lösungsfindung im Gestaltungsprozess abgeleitet. Dieses Indiz wurde als Teil einer methodisch-intuitiven Vorgehensweise für das Planungshandeln beschrieben, um auf die Ambivalenz zwischen holistischer B
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h the establishment of an aerobic biosphere in the Palaeoproterozoic as represented in several palaeobasins and greenstone belts in the Fennoscandian Shield; the Pechenga Greenstone Belt is one of them (Fig. 8.1). From weathering and deposition on Archaean basement overlain by evidence for “Huronian
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Fabian C. Schmidchanges in the biosphere and the geosphere associated with t. .Earth’s present-day environments are the outcome of a 4.5 billion year period of evolution reflecting the interaction of global-scale geological and biological processes punctuated by several extraordinary events and episodes that pertur
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Fabian C. Schmidntal upheavals. Among them, the most important was the establishment of an oxygen-rich atmosphere (sometimes referred to as the Great Oxidation Event) and the emergence of an aerobic biosphere. Associated with this, either incidentally or causally, was a cascade of other prominent, global-scale even
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Fabian C. Schmidrifting of the Archaean cratons of the shield and the commencement of the Svecofennian orogenic events, covering a prolonged inter-orogenic period from c. 2.5 to 1.95 Ga. The focus is on igneous events that took place on and in the Karelian and Kola cratons. These cratons were stabilised by c. 2.6 G
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Fabian C. Schmidlay of plate tectonics and deep mantle dynamics resulting in supercontinental cycles and (super)plume events (Condie et al. 2001; Condie 2004). These processes include the amalgamation, dispersal, collision and geographic position of major land-masses which dictate volcanic and hydrothermal activiti
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Fabian C. Schmidchanges in the biosphere and the geosphere associated with t.Earth’s present-day environments are the outcome of a 4.5 billion year period of evolution reflecting the interaction of global-scale geological and biological processes punctuated by several extraordinary events and episodes that perturbe
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