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  2. Template:Infobox tectonic plate/doc - Wikipedia

    en.wikipedia.org/wiki/Template:Infobox_tectonic...

    Main page; Contents; Current events; Random article; About Wikipedia; Contact us; Pages for logged out editors learn more

  3. Plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Plate_tectonics

    Plate tectonics (from Latin tectonicus, from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building') [1] is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago.

  4. Nappe - Wikipedia

    en.wikipedia.org/wiki/Nappe

    In geology, a nappe or thrust sheet is a large sheetlike body of rock that has been moved more than 2 km (1.2 mi) [1] or 5 km (3.1 mi) [2] [3] above a thrust fault from its original position. Nappes form in compressional tectonic settings like continental collision zones or on the overriding plate in active subduction zones.

  5. Wikipedia : United States Education Program/Courses/Plate ...

    en.wikipedia.org/wiki/Wikipedia:United_States...

    1.1 Printable guides. 1.2 On-wiki tutorials. 1.3 Tutorial videos. 2 Writing articles. ... Wikipedia: United States Education Program/Courses/Plate Tectonics (Alex ...

  6. List of tectonic plates - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plates

    Map showing Earth's principal tectonic plates and their boundaries in detail. These plates comprise the bulk of the continents and the Pacific Ocean.For purposes of this list, a major plate is any plate with an area greater than 20 million km 2 (7.7 million sq mi)

  7. Category:Plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Category:Plate_tectonics

    Download as PDF; Printable version; In other projects Wikimedia Commons; Wikidata item; ... List of tectonic plate interactions; Outline of plate tectonics; A ...

  8. Thin-skinned deformation - Wikipedia

    en.wikipedia.org/wiki/Thin-skinned_deformation

    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. [2]

  9. File:Tectonic plates boundaries detailed-en.svg - Wikipedia

    en.wikipedia.org/wiki/File:Tectonic_plates...

    You are free: to share – to copy, distribute and transmit the work; to remix – to adapt the work; Under the following conditions: attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses ...

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