“…For example, such scenarios typically arise in seismics where at a given location one typically records a temporal signal of certain length [14], [10]. In this case one is given observations X(i, j, :) at indices (i, j) 2 ⌦, i 2 {1, 2, ..., n 1 }, j 2 {1, 2, ..., n 2 }, where ⌦ denotes the sampling set.…”