Titlebook: Web Reasoning and Rule Systems; 7th International Co Wolfgang Faber,Domenico Lembo Conference proceedings 2013 Springer-Verlag Berlin Heide

Flinch

Amélie Gheerbrant,Leonid Libkin,Cristina SirangeloThe environmental features of this area were identified in some small excavations, and also by a comparison and correlation to GPR reflection profiles and magnetic readings across a large buried landscape. The individual geological units that allowed for a regional environmental landscape analysis c

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ULCER

Diego Calvanese,Giuseppe De Giacomo,Marco Montali,Fabio Patriziirical case studies in this field remain deeply entrenched in static push-pull frameworks and tend to reproduce simplistic causal relationships. Drawing on results from an interdisciplinary research project in Mali and Senegal, the chapter presents a methodological approach that emanates from past a

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David Carral,Cong Wang,Pascal Hitzlerabout in themselves their own necessary and inseparable features. In this paper, I propose that self-agency should be understood as an attempt to clarify the relationship between what is necessary but still accidental, and what is essential. I explore this view in the context of two objections again

chance

Daniel Fleischhacker,Christian Meilicke,Johanna Völker,Mathias Niepertn of Bhongir watershed nearer to the Greater Hyderabad. A total of thirty-eight groundwater samples were collected and analysed for important physicochemical parameters, anions and cations. The analytical data of alkalis (Na. and K.) and alkaline earths (Ca. and Mg.), reveal that high concentration

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n 1971; David 1977, 1986; Isaak and Srivastava 1989; Kitanidis 1997). In recent years, these tools have developed from research topics into basic techniques in the design and, such as mining, geology and hydrology, among others. The aim of this chapter is to present application of geostatistical too

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Víctor Gutiérrez-Basulto,Yazmín Ibañez-García,Roman Kontchakov,Egor V. Kostylevrphology. Willey, Chichester, p 562, [.]; Gams (2004) Kras v Sloveniji v prostoru in času. Inštitut za raziskovanje krasa ZRC SAZU, Postojna, p 515,, [.]; Goldscheider and Drew (eds) (2007) Methods in Karst hydrogeology. Taylor & Francis, Leiden, p 264, .). Slovenia is rich in both. Soluble carbonat

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Thomas Eiter,Michael Fink,Daria Stepanova pegmatite, epidote, quartz veins and dolerite dykes traverse the granite. There are three types of fracture patterns (Fig. 1) in the area, viz. (i) mineralised or weathering fractures, (ii) fractures traversed by dykes, and (iii) late-stage fractures represented by joints. The vertical fracture pat

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