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- Q17152600 subject Q2945759.
- Q17152600 subject Q7037486.
- Q17152600 abstract "Tilted block faulting, also called rotational block faulting, is a mode of structural evolution in extensional tectonic events, a result of tectonic plates stretching apart. When the upper lithospheric crust experiences extensional pressures, the brittle crust fractures, creating detachment faults. These normal faults express themselves on a regional scale; upper crust fractures into tilted fault blocks, and ductile lower crust ascends. This results in uplift, cooling, and exhumation of ductily deformed deeper crust. The large unit of tilted blocks and associated crust can help form an integral part of metamorphic core complexes and can occur on both continental and oceanic crust.".
- Q17152600 thumbnail Tilted_Blocks.png?width=300.
- Q17152600 wikiPageWikiLink Q102416.
- Q17152600 wikiPageWikiLink Q148.
- Q17152600 wikiPageWikiLink Q178543.
- Q17152600 wikiPageWikiLink Q188719.
- Q17152600 wikiPageWikiLink Q1925019.
- Q17152600 wikiPageWikiLink Q211702.
- Q17152600 wikiPageWikiLink Q2213536.
- Q17152600 wikiPageWikiLink Q2945759.
- Q17152600 wikiPageWikiLink Q3236743.
- Q17152600 wikiPageWikiLink Q42045.
- Q17152600 wikiPageWikiLink Q42278.
- Q17152600 wikiPageWikiLink Q46.
- Q17152600 wikiPageWikiLink Q47089.
- Q17152600 wikiPageWikiLink Q5265562.
- Q17152600 wikiPageWikiLink Q5641608.
- Q17152600 wikiPageWikiLink Q5906565.
- Q17152600 wikiPageWikiLink Q7037486.
- Q17152600 wikiPageWikiLink Q749565.
- Q17152600 wikiPageWikiLink Q80026.
- Q17152600 wikiPageWikiLink Q816.
- Q17152600 wikiPageWikiLink Q83296.
- Q17152600 wikiPageWikiLink Q849953.
- Q17152600 wikiPageWikiLink Q858847.
- Q17152600 comment "Tilted block faulting, also called rotational block faulting, is a mode of structural evolution in extensional tectonic events, a result of tectonic plates stretching apart. When the upper lithospheric crust experiences extensional pressures, the brittle crust fractures, creating detachment faults. These normal faults express themselves on a regional scale; upper crust fractures into tilted fault blocks, and ductile lower crust ascends.".
- Q17152600 label "Tilted block faulting".
- Q17152600 depiction Tilted_Blocks.png.