syntactical transform - Definition. Was ist syntactical transform
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Was (wer) ist syntactical transform - definition

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
  • Diagram showing a transform fault with two plates moving in opposite directions
  • Down to down NEW
  • Spreading center and strips
  • Spreading centers constant
  • Spreading to Down NEW
  • Spreading to upper NEW
  • Upper to down NEW
  • Upper to upper

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

Wikipedia

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.