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Τι (ποιος) είναι functional transform - ορισμός

PLATE BOUNDARY WHERE THE MOTION IS PREDOMINANTLY HORIZONTAL

Transform-fault; Transform boundary; Transform fault boundary; Transform margin; Conservative plate boundaries; Conservative boundary; Transform faults; Transform Faults; Transform plate boundary; Transform plate; Transverse fault; Transform Margin; Transform Boundaries; Conservative plate boundary; Transform boundry; Transform Boundary; Strike-slip boundary

Z-transform

MATHEMATICAL TRANSFORM WHICH CONVERTS SIGNALS FROM THE TIME DOMAIN TO THE FREQUENCY DOMAIN

Z transform; Laurent transform; Bilateral Z-transform; Bilateral z-transform; Z Transform; Z-domain; Z-transformation

In mathematics and signal processing, the Z-transform converts a discrete-time signal, which is a sequence of real or complex numbers, into a complex frequency-domain (z-domain or z-plane) representation.

https://en.wikipedia.org/wiki/Z-transform

Penrose transform

COMPLEX ANALOGUE OF THE RADON TRANSFORM THAT RELATES MASSLESS FIELDS ON SPACETIME TO COHOMOLOGY OF SHEAVES ON COMPLEX PROJECTIVE SPACE

Penrose-Ward transform; Ward transform; Penrose–Ward transform; Ward correspondence; Twistor transform

In theoretical physics, the Penrose transform, introduced by , is a complex analogue of the Radon transform that relates massless fields on spacetime to cohomology of sheaves on complex projective space. The projective space in question is the twistor space, a geometrical space naturally associated to the original spacetime, and the twistor transform is also geometrically natural in the sense of integral geometry.

https://en.wikipedia.org/wiki/Penrose_transform

transform fault

¦ noun Geology a strike-slip fault occurring at the boundary between two plates of the earth's crust.

Βικιπαίδεια

Transform fault

A transform boundary occurs when two tectonic plates move past one another. Shear stress operates at transform boundaries, which involves sliding motion. No lithosphere is destroyed or created, and mountain chains are not built at transform boundaries. They accommodate the lateral offset between segments of divergent boundaries, forming a zigzag pattern. This is a result of oblique seafloor spreading where the direction of motion is not perpendicular to the trend of the overall divergent boundary. A smaller number of such faults are found on land, although these are generally better-known, such as the San Andreas Fault and North Anatolian Fault.

https://en.wikipedia.org/wiki/Transform fault