Download e-book for kindle: A Cauchy problem in nonlinear heat conduction by De Lillo S., Lupo G., Sanchini G.

By De Lillo S., Lupo G., Sanchini G.

A Cauchy challenge at the semiline for a nonlinear diffusion equation is taken into account, with a boundary such as a prescribed thermal conductivity on the beginning. the matter is mapped right into a relocating boundary challenge for the linear warmth equation with a Robin-type boundary . this kind of challenge is then diminished to a linear imperative Volterra equation of II variety which admits a special answer.

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HALVORSEN, E. 1992. BALTICA—a synopsis of Vendian-Permian palaeomagnetic data and their palaeotectonic implications. Earth-Science Reviews, 33, 133-152. , SVENSSON, I. & WALDERHAUG, H. J. 1993. Palaeogeographic significance of midSilurian palaeomagnetic results from southern Britain: major revision of the apparent polar wander path for eastern Avalonia. Geophysical Journal International, 113, 651-668. TRENCH, A. & TORSVIK, T. H. 1991. A revised Paleozoic apparent polar wander path for south Britain (eastern Avalonia).

Middle Devonian to early Tournaisian limestone turbidites are intercalated with shales and one Tournaisian sandstone member with Caledonian mica ages (Huckriede et al 1998). These are overlain by Famennian to early Visean greywackes (Bender & Homrighausen 1979). 'Hessische Schieferserie'. This unit occupies a structural position between the parautochthon of the Lahn Syncline and the Giessen Nappe. It contains early Devonian sandstones overlain by middle to late Devonian hemipelagic shales and limestones, and Tournaisian radiolarian cherts (Bender 1965; Kegel 1933).

Horre-Gommern Zone, SE part. Middle Devonian to early Tournaisian limestone turbidites are intercalated with shales and one Tournaisian sandstone member with Caledonian mica ages (Huckriede et al 1998). These are overlain by Famennian to early Visean greywackes (Bender & Homrighausen 1979). 'Hessische Schieferserie'. This unit occupies a structural position between the parautochthon of the Lahn Syncline and the Giessen Nappe. It contains early Devonian sandstones overlain by middle to late Devonian hemipelagic shales and limestones, and Tournaisian radiolarian cherts (Bender 1965; Kegel 1933).

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A Cauchy problem in nonlinear heat conduction by De Lillo S., Lupo G., Sanchini G.


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