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Wat (wie) is tectonics$81949$ - definitie
PROCESS BY WHICH MATERIAL IS ADDED TO A TECTONIC PLATE OR A LANDMASS
Docking (geology); Docking (tectonics); Co-accretion
Tectonics of Mars
![Map of crustal magnetic anomaly distribution on Mars, courtesy of [http://www.nasa.gov/centers/goddard/news/topstory/2005/mgs_plates.html/ NASA], 2005.](https://commons.wikimedia.org/wiki/Special:FilePath/Mars Crustal Magnetism MGS.png?width=200 "Map of crustal magnetic anomaly distribution on Mars, courtesy of [http://www.nasa.gov/centers/goddard/news/topstory/2005/mgs_plates.html/ NASA], 2005.")
![Satellite imagery of the Valles Marineris trough system, showing an interpreted large scale strike-slip fault system running along its length.<ref name="Yin" /> Relative fault motion is suggested in part by the offset rim of an old impact basin. Image modified from [http://www.nasa.gov/ NASA]/MOLA Science Team.](https://commons.wikimedia.org/wiki/Special:FilePath/VallesMarinerisOffsetImpactBasin.png?width=200 "Satellite imagery of the Valles Marineris trough system, showing an interpreted large scale strike-slip fault system running along its length.<ref name=\"Yin\" /> Relative fault motion is suggested in part by the offset rim of an old impact basin. Image modified from [http://www.nasa.gov/ NASA]/MOLA Science Team.")
![Geological map of the region around the Tharsis plateau. Extensional and compressional features – e.g., graben and wrinkle ridges – have been mapped and are visible in the image. ([http://pubs.usgs.gov/sim/3292/ USGS], 2014).<ref name="MarsMap" />](https://commons.wikimedia.org/wiki/Special:FilePath/WrinkleRidgesAndGrabensMars.png?width=200 "Geological map of the region around the Tharsis plateau. Extensional and compressional features – e.g., graben and wrinkle ridges – have been mapped and are visible in the image. ([http://pubs.usgs.gov/sim/3292/ USGS], 2014).<ref name=\"MarsMap\" />")
Mars Tectonics; Martian tectonics
Like the Earth, the crustal properties and structure of the surface of Mars are thought to have evolved through time; in other words, as on Earth, tectonic processes have shaped the planet. However, both the ways this change has happened and the properties of the planet's lithosphere are very different when compared to the Earth.
Volcano tectonics
User:Valerio Acocella/Volcano-Tectonics; Volcano-Tectonics
Volcano tectonics is a scientific field that uses the techniques and methods of structural geology, tectonics, and physics to analyse and interpret physical processes and the associated deformation in volcanic areas, at any scale.
Thrust tectonics
![thin-skinned thrust zone]]](https://commons.wikimedia.org/wiki/Special:FilePath/Compressional decollement.svg?width=200 "thin-skinned thrust zone]]")
TECTONIC PROCESSES ASSOCIATED WITH THE SHORTENING AND THICKENING OF THE CRUST
Crustal shortening; Crustal thickening
Thrust tectonics or contractional tectonics is concerned with the structures formed by, and the tectonic processes associated with, the shortening and thickening of the crust or lithosphere. It is one of the three main types of tectonic regime, the others being extensional tectonics and strike-slip tectonics.
Wikipedia
Accretion (geology)
Accretion, in geology, is a process by which material is added to a tectonic plate at a subduction zone, frequently on the edge of existing continental landmasses. The added material may be sediment, volcanic arcs, seamounts, oceanic crust or other igneous features.
