Titlebook: Resilience, Robustness, and Vulnerability of Transport Systems; Analysis, Modelling, Milan Jani? Book 2022 The Editor(s) (if applicable) an

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Milan Jani?anges made mainly of transitional basalts and some differentiated lavas emitted along well-defined open fissures. The mainly silicic and pyroclastic volcanoes, with associated minor basalts, generally with calderas, located along the margins of the depression. The transversal volcanic ranges, made o

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Milan Jani?as well as in central Afar mark the first event (20 to 24 My). It is followed by a trap basaltic unit itself followed by a major rhyolitic phase (Mabla formation 15 to 9 My) marked by important normal faulting and erosion, before a basaltic trap series (Dalha formation 8 to 4 My) covered this unit i

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ctural scale, one sees the similarity in their natures. In clays, the tetrahedra are arranged in a two-dimensional planar layer; in siliceous formations, they are arranged spatially in a three-dimensional lattice. This is the fundamental difference for the specialist in crystalline structures, but f

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Resilience, Robustness, and Vulnerability of Transport SystemsAnalysis, Modelling,

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https://doi.org/10.1007/978-3-031-13040-3Transport Systems; Performances and Indicators; Disruptive Events; Resilience; Transport Analysis; Transp

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978-3-031-13042-7The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerl