scholarly journals The circumcentered-reflection method achieves better rates than alternating projections

Author(s):  
Reza Arefidamghani ◽  
Roger Behling ◽  
Yunier Bello-Cruz ◽  
Alfredo N. Iusem ◽  
Luiz-Rafael Santos
1995 ◽  
Vol 5 (1) ◽  
pp. 3-5 ◽  
Author(s):  
Kwang-Hyun Baek ◽  
He-Young Sung ◽  
Wee Sang Park
Keyword(s):  

Author(s):  
Carlo Alberto De Bernardi ◽  
Enrico Miglierina

AbstractThe 2-sets convex feasibility problem aims at finding a point in the nonempty intersection of two closed convex sets A and B in a Hilbert space H. The method of alternating projections is the simplest iterative procedure for finding a solution and it goes back to von Neumann. In the present paper, we study some stability properties for this method in the following sense: we consider two sequences of closed convex sets $$\{A_n\}$$ { A n } and $$\{B_n\}$$ { B n } , each of them converging, with respect to the Attouch-Wets variational convergence, respectively, to A and B. Given a starting point $$a_0$$ a 0 , we consider the sequences of points obtained by projecting on the “perturbed” sets, i.e., the sequences $$\{a_n\}$$ { a n } and $$\{b_n\}$$ { b n } given by $$b_n=P_{B_n}(a_{n-1})$$ b n = P B n ( a n - 1 ) and $$a_n=P_{A_n}(b_n)$$ a n = P A n ( b n ) . Under appropriate geometrical and topological assumptions on the intersection of the limit sets, we ensure that the sequences $$\{a_n\}$$ { a n } and $$\{b_n\}$$ { b n } converge in norm to a point in the intersection of A and B. In particular, we consider both when the intersection $$A\cap B$$ A ∩ B reduces to a singleton and when the interior of $$A \cap B$$ A ∩ B is nonempty. Finally we consider the case in which the limit sets A and B are subspaces.


Geophysics ◽  
1967 ◽  
Vol 32 (3) ◽  
pp. 411-413 ◽  
Author(s):  
Edward A. Flinn

Since the invention of seismic prospecting more than fifty years ago, significant developments have occurred at an ever increasing rate. Individual opinions would differ about the relative importance of many of these: invention of the reflection method, perfection of techniques for automatic display of record sections, introduction of lightweight geophones, fully portable field recording systems, and media for reproducible recording; and the like. Most geophysicists would agree, however, that what has come to be known as the “digital revolution” overshadows most of the earlier developments.


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