Tectonics

This article is about the geologic usage. For the philosophical or architectural usage, see Architectonics.
"Tectonic" redirects here. Not to be confused with Tecktonik (dance), Tectonic (record label), or Tectonics (journal).

Tectonics (from Latin tectonicus; from Ancient Greek τεκτονικός (tektonikós) 'pertaining to building')[1] are the processes that result in the structure and properties of the Earth's crust and its evolution through time.[2][3]

These processes include those of mountain-building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid plates that constitute the Earth's outer shell interact with each other. Principles of tectonics also provide a framework for understanding the earthquake and volcanic belts that directly affect much of the global population.

Tectonic studies are important as guides for economic geologists searching for fossil fuels and ore deposits of metallic and nonmetallic resources. An understanding of tectonic principles can help geomorphologists to explain erosion patterns and other Earth-surface features.[4]

Main types of tectonic regime

Extensional tectonics

Main article: Extensional tectonics

Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere. This type of tectonics is found at divergent plate boundaries, in continental rifts, during and after a period of continental collision caused by the lateral spreading of the thickened crust formed, at releasing bends in strike-slip faults, in back-arc basins, and on the continental end of passive margin sequences where a detachment layer is present.[5][6][7]

Thrust (contractional) tectonics

Main article: Thrust tectonics

Thrust tectonics is associated with the shortening and thickening of the crust, or the lithosphere. This type of tectonics is found at zones of continental collision, at restraining bends in strike-slip faults, and at the oceanward part of passive margin sequences where a detachment layer is present.[8]

Strike-slip tectonics

San Andreas transform fault on the Carrizo Plain
Main article: Strike-slip tectonics

Strike-slip tectonics is associated with the relative lateral movement of parts of the crust or the lithosphere. This type of tectonics is found along oceanic and continental transform faults which connect offset segments of mid-ocean ridges. Strike-slip tectonics also occurs at lateral offsets in extensional and thrust fault systems. In areas involved with plate collisions strike-slip deformation occurs in the over-riding plate in zones of oblique collision and accommodates deformation in the foreland to a collisional belt.[9]

Plate tectonics

Main article: Plate tectonics
The Tectonic Network of the Earth. Legend: Brown: Terrane (microplate) boundaries in the continents and Mobile Belts, Cyan: Terranes of the Oceanic Plates, Blue: Oceanic transform faults; Red and orange: Fault zones in the Continental and Mountain belt domain; Purple: Main subduction zones and suture zones; Green: Continental margins

In plate tectonics, the outermost part of the Earth known as the lithosphere (the crust and uppermost mantle) act as a single mechanical layer. The lithosphere is divided into separate "plates" that move relative to each other on the underlying, relatively weak asthenosphere in a process ultimately driven by the continuous loss of heat from the Earth's interior. There are three main types of plate boundaries: divergent, where plates move apart from each other and new lithosphere is formed in the process of sea-floor spreading; transform, where plates slide past each other, and convergent, where plates converge and lithosphere is "consumed" by the process of subduction. Convergent and transform boundaries are responsible for most of the world's major (Mw > 7) earthquakes. Convergent and divergent boundaries are also the site of most of the world's volcanoes, such as around the Pacific Ring of Fire. Most of the deformation in the lithosphere is related to the interaction between plates at or near plate boundaries. The latest studies, based on the integration of available geological data, and satellite imagery and Gravimetric and magnetic anomaly datasets have shown that the crust of the Earth is dissected by thousands of different types of tectonic elements which define the subdivision into numerous smaller microplates which have amalgamated into the larger Plates.[10]

Other fields of tectonic studies

Salt tectonics

Main article: Salt tectonics

Salt tectonics is concerned with the structural geometries and deformation processes associated with the presence of significant thicknesses of rock salt within a sequence of rocks. This is due both to the low density of salt, which does not increase with burial, and its low strength.[11]

Neotectonics

Main article: Neotectonics

Neotectonics is the study of the motions and deformations of the Earth's crust (geological and geomorphological processes) that are current or recent in geological time. The term may also refer to the motions and deformations themselves. The corresponding time frame is referred to as the neotectonic period. Accordingly, the preceding time is referred to as palaeotectonic period.[12]

Tectonophysics

Main article: Tectonophysics

Tectonophysics is the study of the physical processes associated with deformation of the crust and mantle from the scale of individual mineral grains up to that of tectonic plates.[13]

Seismotectonics

Main article: Seismotectonics

Seismotectonics is the study of the relationship between earthquakes, active tectonics, and individual faults in a region. It seeks to understand which faults are responsible for seismic activity in an area by analysing a combination of regional tectonics, recent instrumentally recorded events, accounts of historical earthquakes, and geomorphological evidence. This information can then be used to quantify the seismic hazard of an area.[14]

Impact tectonics

Impact tectonics is the study of modification of the lithosphere through high velocity impact cratering events.[15]

Planetary tectonics

Techniques used in the analysis of tectonics on Earth have also been applied to the study of the planets and their moons.[3]

See also

References

  1. ^ Harper, Douglas. "tectonic". Online Etymology Dictionary.
  2. ^ Geologists (as distinct from architects) may define tectonics as "the architecture of the Earth's crust" - O'Hara, Kieran D. (19 April 2018). A Brief History of Geology. Cambridge: Cambridge University Press. ISBN 9781107176188. Retrieved 23 March 2023. The words tectonics and architecture are derived from the same Greek root, and tectonics is defined as the architecture of the Earth's crust.
  3. ^ a b The field of planetary tectonics extends the concept of tectonics to studying non-terrestrial bodies such as other planets and moons: Watters, Thomas R.; Schultz, Richard A. (2010). "Planetary tectonics: introduction". In Watters, Thomas R.; Schultz, Richard A. (eds.). Planetary Tectonics. Cambridge Planetary Science, ISSN 0265-3044 - Volume 11. Cambridge: Cambridge University Press. p. 2. ISBN 9780521765732. Retrieved 23 March 2023. Since the 1960s, an armada of exploratory spacecraft have identified widespread evidence of tectonism on all the terrestrial planets, most of the satellites of the outer planets, and on a number of asteroids. Tectonic landforms on large and small bodies in the solar system are as ubiquitous as impact craters.
  4. ^ Anderson, Robert S.; Burbank, Douglas W. (2 November 2011) [2001]. "Rates of erosion and uplift". Tectonic Geomorphology (2 ed.). Chichester, West Sussex: John Wiley & Sons. ISBN 9781444345049. Retrieved 23 March 2023.
  5. ^ Armijo, R.; Meyer, B.; Navarro, S.; King, G.; Barka, A. (2002), "Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian Fault?" (PDF), Terra Nova, 14 (2), Wiley-Blackwell: 80–86, Bibcode:2002TeNov..14...80A, CiteSeerX 10.1.1.546.4111, doi:10.1046/j.1365-3121.2002.00397.x, S2CID 49553634
  6. ^ Sdrolias, M; Muller, R.D. (2006). "Controls on back-arc basin formations". Geochemistry, Geophysics, Geosystems. 7 (4): Q04016. Bibcode:2006GGG.....7.4016S. doi:10.1029/2005GC001090. S2CID 129068818.
  7. ^ Brun, J,-P.; Fort, X. (2011). "Salt tectonics at passive margins: Geology versus models". Marine and Petroleum Geology. 28 (6): 1123–1145. Bibcode:2011MarPG..28.1123B. doi:10.1016/j.marpetgeo.2011.03.004.{cite journal}: CS1 maint: multiple names: authors list (link)
  8. ^ Butler, R.; Bond, C. (2020). "Chapter 9 - Thrust systems and contractional tectonics". In Scarselli, N.; Adam, J.; Chiarella, D. (eds.). Principles of Geologic Analysis. Regional Geology and Tectonics. Vol. 1 (2 ed.). Elsevier. pp. 149–167. doi:10.1016/B978-0-444-64134-2.00008-0. ISBN 9780444641359.
  9. ^ Burg, J.-P. (2017). "Strike-slip and Oblique-slip tectonics" (PDF). Retrieved 26 September 2022.
  10. ^ van Dijk, J.P. (2023); The New Global Tectonic Map - Analyses and Implications. Terra Nova, 2023, 27 pp. doi:10.1111/TER.12662
  11. ^ Hudec, M.R.; Jackson, M.P.A. (2007). "Terra infirma: Understanding salt tectonics". Earth-Science Reviews. 82 (1–2): 1–28. doi:10.1016/j.earscirev.2007.01.001.
  12. ^ "Encyclopedia of Coastal Science" (2005), Springer, ISBN 978-1-4020-1903-6, Chapter 1: "Tectonics and Neotectonics" doi:10.1007/1-4020-3880-1
  13. ^ Foulger, Gillian R. (2021), "The Plate Theory for Volcanism", Encyclopedia of Geology, Elsevier, pp. 879–890, doi:10.1016/b978-0-08-102908-4.00105-3, ISBN 978-0-08-102909-1, retrieved 23 October 2023
  14. ^ E. Boschi, E.; Mantovani, E.; Morelli, A., eds. (2012). "A review of the Eastern Alps - Northern Dinarides Seismotectonics". Recent Evolution and Seismicity of the Mediterranean Region. Springer. ISBN 9789401120166.
  15. ^ Koeberl, C., Henkel, H., eds. (2005). Impact Tectonics. Impact Studies. Springer Berlin Heidelberg. doi:10.1007/3-540-27548-7. ISBN 978-3-540-24181-2.

Further reading

Look up tectonics or tectonic in Wiktionary, the free dictionary.