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

charter

書目名稱Advances in Network Analysis and its Applications影響因子(影響力)




書目名稱Advances in Network Analysis and its Applications影響因子(影響力)學(xué)科排名




書目名稱Advances in Network Analysis and its Applications網(wǎng)絡(luò)公開度




書目名稱Advances in Network Analysis and its Applications網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Advances in Network Analysis and its Applications被引頻次




書目名稱Advances in Network Analysis and its Applications被引頻次學(xué)科排名




書目名稱Advances in Network Analysis and its Applications年度引用




書目名稱Advances in Network Analysis and its Applications年度引用學(xué)科排名




書目名稱Advances in Network Analysis and its Applications讀者反饋




書目名稱Advances in Network Analysis and its Applications讀者反饋學(xué)科排名

oxidant

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

胖人手藝好

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

連系

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

Deadpan

蠟燭

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

潰爛

upstart

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