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- [1] Moyal quantization of sdiff(T2k/N), q-deformation, and q-moyal bracket[J]. INTERNATIONAL JOURNAL OF THEORETICAL PHYSICS, 1998, 37 (03) : 1011 - 1017El Kinani, EHOuarab, A
- [2] COMMENT ON Q-DEFORMATION IN 2ND QUANTIZATION PROCEDURE[J]. PROGRESS OF THEORETICAL PHYSICS, 1993, 90 (05): : 1149 - 1153ODAKA, K
- [7] The Best Article Award 2013 of the Society of Resource Geology was Presented to K. Adomako-Ansah, T. Mizuta, N. Q. Hammond, D. Ishiyama, T. Ogata and H. Chiba, for the Following Paper: Gold mineralization in banded iron formation in the Amalia greenstone belt, South Africa: a mineralogical and sulfur isotope study. Resource Geology, 63(2), 119-140[J]. RESOURCE GEOLOGY, 2014, 64 (04) : 395 - 395Urabe, Tetsuro
- [8] Functions f from Fn p, n=2m, to Z pk for which the character sum Hk f (pt, u) = ∼ x.Fn p. ptf (x) pk. u. x p (where.q=e2pi/ q is a q-th root of unity), has absolute value pm for all u. Fn p and 0=t = k-1, induce relative difference sets in Fn p x Z pk hence are called bent. Functions only necessarily satisfying |Hk f (1, u)| = pm are called generalized bent. We show that with spreads we not only can construct a variety of bent and generalized bent functions, but also can design functions from Fn p to Zpm satisfying |Hm f (pt, u)| = pm if and only if t. T for any T. {0, 1..., m-1}. A generalized bent function can also be seen as a Boolean (p-ary) bent function together with a partition of Fn p with certain properties. We show that the functions from the completed Maiorana-McFarland class are bent functions, which allow the largest possible partitions.[J]. CRYPTOGRAPHY AND COMMUNICATIONS-DISCRETE-STRUCTURES BOOLEAN FUNCTIONS AND SEQUENCES, 2019, 11 (06): : 1233 - 1245Meidl, WilfriedPott, Alexander