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  2. Diastrophism - Wikipedia

    en.wikipedia.org/wiki/Diastrophism

    Diastrophism is the process of deformation of the Earth's crust which involves folding and faulting. Diastrophism can be considered part of geotectonics. The word is derived from the Greek διαστροϕή diastrophḗ 'distortion, dislocation'. [1]

  3. Collision zone - Wikipedia

    en.wikipedia.org/wiki/Collision_zone

    A collision zone occurs when tectonic plates meet at a convergent boundary both bearing continental lithosphere.As continental lithosphere is usually not subducted due to its relatively low density, the result is a complex area of orogeny involving folding and thrust faulting as the blocks of continental crust pile up above the subduction zone.

  4. Fold mountains - Wikipedia

    en.wikipedia.org/wiki/Fold_mountains

    Fold mountains form in areas of thrust tectonics, such as where two tectonic plates move towards each other at convergent plate boundary.When plates and the continents riding on them collide or undergo subduction (that is – ride one over another), the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak ...

  5. Thin-skinned deformation - Wikipedia

    en.wikipedia.org/wiki/Thin-skinned_deformation

    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. [1]

  6. Detachment fold - Wikipedia

    en.wikipedia.org/wiki/Detachment_fold

    The definition of disharmonic folds (below) however, incorporates many types of symmetric folds over a larger area encompassing many geometries and attributes of the basic models and may be better suited to the application of these models. Figure 3. Disharmonic folding of a detachment fold using a symmetric geometric fold as a model.

  7. Detachment fault - Wikipedia

    en.wikipedia.org/wiki/Detachment_fault

    View of Doso Doyabi, Snake Range, Nevada, which was formed by detachment faulting. A detachment fault is a gently dipping normal fault associated with large-scale extensional tectonics . [ 1 ] Detachment faults often have very large displacements (tens of km) and juxtapose unmetamorphosed hanging walls against medium to high-grade metamorphic ...

  8. Décollement - Wikipedia

    en.wikipedia.org/wiki/Décollement

    Two different types of folding may occur at a décollement. Concentric folding is identified by uniform bed thickness throughout the fold, and is necessarily accompanied by detachment or a décollement as part of the deformation that occurs with a thrust fault. [15] Disharmonic folding does not have uniform bed thickness throughout the fold. [16]

  9. Folding (chemistry) - Wikipedia

    en.wikipedia.org/wiki/Folding_(chemistry)

    In chemistry, folding is the process by which a molecule assumes its shape or conformation. The process can also be described as intramolecular self-assembly , a type of molecular self-assembly , where the molecule is directed to form a specific shape through noncovalent interactions , such as hydrogen bonding , metal coordination, hydrophobic ...