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H. Eugene Stanley

Researcher at Boston University

Publications -  1208
Citations -  134813

H. Eugene Stanley is an academic researcher from Boston University. The author has contributed to research in topics: Complex network & Phase transition. The author has an hindex of 154, co-authored 1190 publications receiving 122321 citations. Previous affiliations of H. Eugene Stanley include University of North Carolina at Chapel Hill & Wesleyan University.

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Statistical Properties of Cross-Correlation in the Korean Stock Market

TL;DR: The authors investigated the statistical properties of the correlation matrix between individual stocks traded in the Korean stock market using the random matrix theory (RMT) and observed how these affect the portfolio weights in the Markowitz portfolio theory.
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Recent results on the connection between thermodynamics and dynamics in supercooled water.

TL;DR: Evidence is found suggesting that the glass transition temperature of water may be significantly higher than previously reported, but is still consistent with recent measurements, and the hypothesis that the dynamical behavior of deeply supercooled water undergoes a crossover from 'fragile' to 'strong' behavior is discussed.
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Percolation theory and fragmentation measures in social networks

TL;DR: It is found that for a network obtained after removal of a fraction q of nodes above criticality, P∞≈(1-F)1/2, the fragmentation measure F better reflects the actual fragmentation and thus one can improve significantly the fragmentation of the network.
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Time-varying lead-lag structure between the crude oil spot and futures markets

TL;DR: In this paper, a nonparametric and nonlinear symmetric thermal optimal path (TOPS) method was employed to determine the time-dependent lead-lag relationship between two time series.
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Liquid water: A very complex fluid

TL;DR: In this paper, a qualitative interpretation in terms of percolation concepts is given for H2O and the Gibbs potential G(P, T) and the equation of state V (P,T) for water, both of which are consistent with the possible continuity of liquid water and the amorphous forms of solid water.