as an example, If your visibility of a *Reconstructed Geometries* layer is turned off although the layer remains enabled then attribute geometries are still reconstructed internally by GPlates for that layer Gplatehar (they are just not displayed).
The users may choose to visualise their 3D volume via a Cross part. A Cross section is usually a 2nd vertical slice in the scalar field. Any present floor geometries (
This is certainly also The explanation why a reconstructed world raster addresses your entire world At this time-working day but addresses a progressively lesser space in the world as you reconstruct back again in time.
) can be employed as being the supply of these cross sections. These polylines/polygons are extruded down Within the Earth and map the 3D scalar subject values (that intersect these extruded surfaces) to colors.
layer might be the default and you'll inform which a person would be the default since it will be the only layer With all the icon obvious beside the layer identify.
so that you can rotate the current-day geometries of characteristics, a rotation hierarchy is necessary and this is obtained by connecting a Reconstruction Tree layer.
just one deviation window is achievable, where you have one particular isosurface at value V and its two semi-transparent deviation isosurfaces at 'V+dev1' and 'V-dev2'.
A double deviation window is additionally probable, consisting of two one nonoverlapping deviaiton Home windows, which will Each and every be separately configured by isovalue and deviation offset.
Reconstructions are described inside of a relative trend; only one full reconstruction pole defines the motion of 1 plate id (the "shifting" plate id) relative to another (the "fixed" plate id) at a specific instant in geological time.
As talked over earlier In this particular documentation, GPlates works by using the strategy of the Plate ID to ascribe tectonic motion to your attribute. All characteristics utilizing the very same plate ID transfer in unison when reconstructed back through time.
Plate IDs tend not to correspond to some physical tectonic plate, While they may depict the movement of functions that are on that Bodily plate. Plate IDs can also be assigned to characterize the motion of items on exactly the same Bodily plate relative to one another - for example, the movement of the island arc caused by back again-arc spreading.
This is actually the default configuration exactly where no input channels are linked (besides the raster attribute itself).
The visibility of each and every layer is usually individually disabled (or enabled) by clicking the icon to your left in the layer identify.
the different exhibit… solutions below Network & Triangulation choices are accustomed to display unique components of the triangulation produced while in the deforming region. they are generally debugging and visualisation aids.