考古学 发表于 2025-3-23 11:24:21
Substitutions in Dynamics, Arithmetics and CombinatoricsHAVOC 发表于 2025-3-23 15:34:01
Automatic sequences and transcendenceossible to characterize algebraicity in a simple way: a formal power series is algebraic if and only if the sequence of its coefficients is automatic; this criterion is known as Christol, Kamae, Mendès France, and Rauzy’s theorem. In a similar vein, the continued fraction expansion of an algebraic nseroma 发表于 2025-3-23 20:21:04
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es of solids, particularly near the melting point. The results have impacts in areas ranging from volcanic processes, through the structure of the deep Earth, to fluid-saturated porous media..978-3-319-38063-6978-3-319-03098-2Series ISSN 2190-5053 Series E-ISSN 2190-5061手铐 发表于 2025-3-24 02:35:27
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emente verschiedene oder modifizierte Stoffgesetze anzuwenden sind. Die Möglichkeit einer rheologischen Behandlung solcher Gefüge hängt letztlich davon ab, wieweit diese nach gefügeanalytischer Voruntersuchung als statistische Kontinua zu betrachten sind, oder ob mathematische Wege aufgezeigt werden浸软 发表于 2025-3-24 15:47:36
n-negative. Outside of the contact area . = 0. The problem is to find the contact pressure . and the shape of the contact region . for a given depth of indentation, or a given total force applied to the punch. In general, the governing equation can be reduced to the following integral equation:.in w药物 发表于 2025-3-24 22:20:40
mineral mechanics.Includes applications to igneous, metamorOur understanding of the rheological and seismic properties of the Earth’s interior relies on interpreting geophysical observations using mineral physics data. The complexity of natural materials complicates these interpretations, but hereextinguish 发表于 2025-3-25 01:37:38
mineral mechanics.Includes applications to igneous, metamorOur understanding of the rheological and seismic properties of the Earth’s interior relies on interpreting geophysical observations using mineral physics data. The complexity of natural materials complicates these interpretations, but here