Übersetzung und Analyse von Wörtern durch künstliche Intelligenz
Auf dieser Seite erhalten Sie eine detaillierte Analyse eines Wortes oder einer Phrase mithilfe der besten heute verfügbaren Technologie der künstlichen Intelligenz:
- wie das Wort verwendet wird
- Häufigkeit der Nutzung
- es wird häufiger in mündlicher oder schriftlicher Rede verwendet
- Wortübersetzungsoptionen
- Anwendungsbeispiele (mehrere Phrasen mit Übersetzung)
- Etymologie
Was (wer) ist crustal$17886$ - definition
![thin-skinned thrust zone]]](https://commons.wikimedia.org/wiki/Special:FilePath/Compressional decollement.svg?width=200 "thin-skinned thrust zone]]")
![Ga]] represents the onset of subduction and plate tectonics. Modified from <ref name=":3" />](https://commons.wikimedia.org/wiki/Special:FilePath/Growthcurve.png?width=200 "Ga]] represents the onset of subduction and plate tectonics. Modified from <ref name=\":3\" />")
![upper mantle]]) olivine would crystallise.](https://commons.wikimedia.org/wiki/Special:FilePath/Phasediagram.png?width=200 "upper mantle]]) olivine would crystallise.")
![Kennedy Developmental Road]].](https://commons.wikimedia.org/wiki/Special:FilePath/Kennedy Development Road.jpg?width=200 "Kennedy Developmental Road]].")
![Palaeozoic]] [[impact structure]].](https://commons.wikimedia.org/wiki/Special:FilePath/UpperDiamantinaCrustalAnomaly.png?width=200 "Palaeozoic]] [[impact structure]].")
Wikipedia
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. These match the three types of plate boundary, convergent (thrust), divergent (extensional) and transform (strike-slip). There are two main types of thrust tectonics, thin-skinned and thick-skinned, depending on whether or not basement rocks are involved in the deformation. The principle geological environments where thrust tectonics is observed are zones of continental collision, restraining bends on strike-slip faults and as part of detached fault systems on some passive margins.
