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- Q7784242 subject Q2945759.
- Q7784242 abstract "Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks.The thin-skinned style of deformation is typical of many fold and thrust belts developed in the foreland of a collisional zone or back arc of a continental volcanic arc. This is particularly the case where a good basal decollement exists, usually in a weaker layer like a shale, evaporite, or a zone of high pore fluid pressure. This was first described in Rocky Mountains of the United States, as part of the Sevier Orogeny.In the rock record, this will increase the influence of more surficial rocks, which usually includes sedimentary rocks. Typically, you will see repeated sections of the same rock over and over as thrust faults, coming up from the decollement, stack the same layer on top of itself. The sediments that are created by this type of deformation are typically lithic sandstones.".
- Q7784242 thumbnail SunRiver.JPG?width=300.
- Q7784242 wikiPageWikiLink Q1255282.
- Q7784242 wikiPageWikiLink Q13426043.
- Q7784242 wikiPageWikiLink Q1391957.
- Q7784242 wikiPageWikiLink Q2143968.
- Q7784242 wikiPageWikiLink Q2672013.
- Q7784242 wikiPageWikiLink Q2945759.
- Q7784242 wikiPageWikiLink Q30.
- Q7784242 wikiPageWikiLink Q331927.
- Q7784242 wikiPageWikiLink Q491689.
- Q7784242 wikiPageWikiLink Q496325.
- Q7784242 wikiPageWikiLink Q5463.
- Q7784242 wikiPageWikiLink Q5464261.
- Q7784242 wikiPageWikiLink Q6647903.
- Q7784242 wikiPageWikiLink Q751300.
- Q7784242 wikiPageWikiLink Q7783915.
- Q7784242 wikiPageWikiLink Q7950.
- Q7784242 wikiPageWikiLink Q82480.
- Q7784242 comment "Thin-skinned deformation is a style of deformation in plate tectonics at a convergent boundary which occurs with shallow thrust faults that only involves cover rocks (typically sedimentary rocks), and not deeper basement rocks.The thin-skinned style of deformation is typical of many fold and thrust belts developed in the foreland of a collisional zone or back arc of a continental volcanic arc.".
- Q7784242 label "Thin-skinned deformation".
- Q7784242 depiction SunRiver.JPG.