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The ordinary component of l-isogeny graph of elliptic curves

dc.contributorGraduate Program in Mathematics.
dc.contributor.advisorÖzman, Ekin.
dc.contributor.authorKaytancı, Kübra.
dc.date.accessioned2023-03-16T11:21:44Z
dc.date.available2023-03-16T11:21:44Z
dc.date.issued2017.
dc.description.abstractIn this thesis, our aim is to understand `-volcanoes which are ordinary compo nents of `-isogeny graphs of elliptic curves over finite fields under certain conditions. In 1996, the structure of isogeny graphs of elliptic curves described by David Kohel in his PhD thesis [1]. Later, in 2002 Mireille Fouquet and Francois Morain extended Kohel’s work by defining isogeny volcanoes [2]. Firstly, we give some basic definitions and tools as used throughout this thesis. Then we study the Kohel’s theorem and give a 3-volcano of depth 2 over F409 as an example.
dc.format.extent30 cm.
dc.format.pagesx, 59 leaves ;
dc.identifier.otherMATH 2017 K38
dc.identifier.urihttps://hdl.handle.net/20.500.14908/15298
dc.publisherThesis (M.S.) - Bogazici University. Institute for Graduate Studies in Science and Engineering, 2017.
dc.subject.lcshCurves, Elliptic.
dc.titleThe ordinary component of l-isogeny graph of elliptic curves

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