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Undergraduate Texts in Mathematics, 1982 Transformation Geometry: An Introduction to Symmetry is a modern approach to Euclidean geometry.vii,237 page ...
George E Martin
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Teaching Transformation Geometry With Cabri Geometry Plus II [PDF]
Procedia, Social and Behavioral Sciences, 2012 AbstractThe overall aim of this study is to search whether teaching geometry with Cabri Geometry Plus II software have effects on 7th grade students’ learning transformation geometry in mathematics. In this context, the researcher has used a pre-test and post-test research design with a control group.
Yazlık, Derya Özlem, Ardahan, Halil
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Disformal Transformation in Newton–Cartan Geometry [PDF]
European Physical Journal C, 2016 Newton–Cartan geometry has played a central role in recent discussions of the non-relativistic holography and condensed matter systems. Although the conformal transformation in non-relativistic holography can easily be rephrased in terms of Newton–Cartan
Fang-Fang Yuan
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Geometry of Infinitesimal Harmonic Transformations
Annals of Global Analysis and Geometry, 2003The vector field \(\xi\) is an infinitesimal harmonic transformation in a Riemannian manifold \((M, g)\) if the local one-parameter group of infinitesimal point transformations generated by the vector field \(\xi\) is a group of harmonic transformations.
Sergey Stepanov, Igor Shandra
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Transformations, Regression Geometry and R2
Computational Statistics and Data Analysis, 2003zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Yufen Huang, Norman R Draper
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On the Geometry of a Homogeneous Contact Transformation
2000Let \(M\) be a smooth manifold and \(T^*M\) (resp. \(T^*_0M\)) be its cotangent bundle (resp. cotangent bundle with the zero section removed). A diffeomorphism of \(T^*M\) preserving its canonical contact form is called a homogeneous contact transformation (h.c.t.). In this note, a very particular class of h.c.t. is considered, namely h.c.t. compatible
Antonelli, P. L., Hrimiuc, D.
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Geometry by Its Transformations
Compact Textbooks in MathematicsChristopher Baltus
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Nature, 1980
Asymmetric sea-floor formation at oceanic spreading centre/transform fault intersections is predicted by the steady-state (average) geometry of finite-width transform fault zones. In the central North Atlantic, geological and geophysical data near both small-offset (FAMOUS Fracture Zone B) and large-offset (Kane Fracture Zone) transforms support this ...
Hans Schouten, Jeff Karson, Henry Dick
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Asymmetric sea-floor formation at oceanic spreading centre/transform fault intersections is predicted by the steady-state (average) geometry of finite-width transform fault zones. In the central North Atlantic, geological and geophysical data near both small-offset (FAMOUS Fracture Zone B) and large-offset (Kane Fracture Zone) transforms support this ...
Hans Schouten, Jeff Karson, Henry Dick
openaire +1 more source