Titlebook: Advances in Network Analysis and its Applications; Evangelos Kranakis Book 2013 Springer-Verlag Berlin Heidelberg 2013 Applied Mathematics

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书目名称Advances in Network Analysis and its Applications影响因子(影响力)




书目名称Advances in Network Analysis and its Applications影响因子(影响力)学科排名




书目名称Advances in Network Analysis and its Applications网络公开度




书目名称Advances in Network Analysis and its Applications网络公开度学科排名




书目名称Advances in Network Analysis and its Applications被引频次




书目名称Advances in Network Analysis and its Applications被引频次学科排名




书目名称Advances in Network Analysis and its Applications年度引用




书目名称Advances in Network Analysis and its Applications年度引用学科排名




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书目名称Advances in Network Analysis and its Applications读者反馈学科排名

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CUMB

Systemic Risk in Banking Networks Without Monte Carlo Simulationarticular, they provide a new means of addressing open questions in astrophysics and fundamental physics and for studying black holes: from their formation, evolution and demographics, to the assembly history of galactic structures and the dynamical behaviour of gravitational fields in the strong no

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Systemic Valuation of Banks: Interbank Equilibrium and Contagion of a potentially observable strength and frequency. Theory can at present only give an indication of what sources. be seen, together with limits on their strength and event rate. This review considers both the kind of information we can expect from observations of any particular class of sources, a

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An Open Problemal waves. Several gravitational-wave observational programs, called Pulsar Timing Arrays (PTA), are being pursued around the world. Here we develop a Bayesian inference method for measuring the stochastic gravitational-wave background (GWB) from the PTA data. Our method has several strengths: (1) It

COMA

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longitude 88° to 100° E is one of the most interesting parts of the world. Here large scale thrust movements directed from northwest and southeast have resulted in the formation of Eastern Himalaya (whose highest peak is Namche Barwa (7755 m high) in the north, Naga Hills in the south and Assam-Brah

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Complex Networks and Social Networkspts and formulas for gravity inversion, various isostatic models and their use in determining crustal depth by gravity is described at length and compared and combined with seismic models of crustal depth. The preferred isostatic model is based on Vening Meinesz-Moritz hypothesis with a global isost