342:. 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.
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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
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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
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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
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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.
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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
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299:) act as a single mechanical layer. The lithosphere is divided into separate "plates" that move relative to each other on the underlying, relatively weak
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Salt tectonics is concerned with the structural geometries and deformation processes associated with the presence of significant thicknesses of
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Thrust tectonics is associated with the shortening and thickening of the crust, or the lithosphere. This type of tectonics is found at zones of
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The words tectonics and architecture are derived from the same Greek root, and tectonics is defined as the architecture of the Earth's crust.
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Butler, R.; Bond, C. (2020). "Chapter 9 - Thrust systems and contractional tectonics". In
Scarselli, N.; Adam, J.; Chiarella, D. (eds.).
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in a process ultimately driven by the continuous loss of heat from the Earth's interior. There are three main types of plate boundaries:
216:, at restraining bends in strike-slip faults, and at the oceanward part of passive margin sequences where a detachment layer is present.
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that constitute the Earth's outer shell interact with each other. Principles of tectonics also provide a framework for understanding the
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Watters, Thomas R.; Schultz, Richard A. (2010). "Planetary tectonics: introduction". In
Watters, Thomas R.; Schultz, Richard A. (eds.).
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The field of planetary tectonics extends the concept of tectonics to studying non-terrestrial bodies such as other planets and moons:
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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.
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673:"Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian Fault?"
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strike-slip deformation occurs in the over-riding plate in zones of oblique collision and accommodates deformation in the
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Impact tectonics is the study of modification of the lithosphere through high velocity impact cratering events.
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598:. Cambridge Planetary Science, ISSN 0265-3044 - Volume 11. Cambridge: Cambridge University Press. p. 2.
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van Dijk, J.P. (2023); The New Global
Tectonic Map - Analyses and Implications. Terra Nova, 2023, 27 pp.
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Seismotectonics is the study of the relationship between earthquakes, active tectonics, and individual
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Techniques used in the analysis of tectonics on Earth have also been applied to the study of the
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This article is about the geologic usage. For the philosophical or architectural usage, see
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Brun, J,-P.; Fort, X. (2011). "Salt tectonics at passive margins: Geology versus models".
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Extensional tectonics is associated with the stretching and thinning of the crust or the
836:. Regional Geology and Tectonics. Vol. 1 (2 ed.). Elsevier. pp. 149–167.
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of metallic and nonmetallic resources. An understanding of tectonic principles can help
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caused by the lateral spreading of the thickened crust formed, at releasing bends in
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Hudec, M.R.; Jackson, M.P.A. (2007). "Terra infirma: Understanding salt tectonics".
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The Origin and the
Mechanics of the Forces Responsible for Tectonic Plate Movements
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Earth
Structure – An Introduction to Structural Geology and Tectonics. 2nd edition
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174:. This type of tectonics is found at divergent plate boundaries, in continental
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252:. Strike-slip tectonics also occurs at lateral offsets in extensional and
112:, the growth and behavior of the strong, old cores of continents known as
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633:; Burbank, Douglas W. (2 November 2011) . "Rates of erosion and uplift".
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101:') are the processes that result in the structure and properties of the
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1002:"A review of the Eastern Alps - Northern Dinarides Seismotectonics"
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Neotectonics is the study of the motions and deformations of the
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In plate tectonics, the outermost part of the Earth known as the
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Stanley A. Schumm, Jean F. Dumont and John M. Holbrook (2002)
639:(2 ed.). Chichester, West Sussex: John Wiley & Sons.
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Recent
Evolution and Seismicity of the Mediterranean Region
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E. Boschi, E.; Mantovani, E.; Morelli, A., eds. (2012).
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Active
Tectonics: Earthquakes, Uplift, and Landscape
932:"Encyclopedia of Coastal Science" (2005), Springer,
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Geologists (as distinct from architects) may define
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that directly affect much of the global population.
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37:"Tectonic" redirects here. Not to be confused with
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1035:. Impact Studies. Springer Berlin Heidelberg.
667:Armijo, R.; Meyer, B.; Navarro, S.; King, G.;
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549:as "the architecture of the Earth's crust" -
131:Tectonic studies are important as guides for
116:, and the ways in which the relatively rigid
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817:: CS1 maint: multiple names: authors list (
1098:B.A. van der Pluijm and S. Marshak (2004).
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557:. Cambridge: Cambridge University Press.
391:processes) that are current or recent in
27:Process of evolution of the Earth's crust
867:"Strike-slip and Oblique-slip tectonics"
496:UNESCO world heritage site Glarus Thrust
736:"Controls on back-arc basin formations"
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1104:. New York: W.W. Norton. p. 656.
1029:Koeberl, C., Henkel, H., eds. (2005).
810:
7:
1085:Active Tectonics and Alluvial Rivers
740:Geochemistry, Geophysics, Geosystems
1413:List of tectonic plate interactions
551:O'Hara, Kieran D. (19 April 2018).
971:10.1016/b978-0-08-102908-4.00105-3
842:10.1016/B978-0-444-64134-2.00008-0
734:Sdrolias, M; Muller, R.D. (2006).
151:and other Earth-surface features.
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283:zones; Green: Continental margins
248:which connect offset segments of
108:These processes include those of
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959:"The Plate Theory for Volcanism"
714:10.1046/j.1365-3121.2002.00397.x
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346:Other fields of tectonic studies
256:systems. In areas involved with
202:Thrust (contractional) tectonics
190:, and on the continental end of
105:and its evolution through time.
920:10.1016/j.earscirev.2007.01.001
834:Principles of Geologic Analysis
805:10.1016/j.marpetgeo.2011.03.004
178:, during and after a period of
965:, Elsevier, pp. 879–890,
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155:Main types of tectonic regime
1073:Prentice Hall; 2nd edition,
957:Foulger, Gillian R. (2021),
785:Marine and Petroleum Geology
532:Online Etymology Dictionary
229:San Andreas transform fault
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554:A Brief History of Geology
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1269:Orthographic projection
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1198:Lamé's stress ellipsoid
963:Encyclopedia of Geology
264:to a collisional belt.
43:Tectonic (record label)
636:Tectonic Geomorphology
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220:Strike-slip tectonics
214:continental collision
180:continental collision
166:Extensional tectonics
160:Extensional tectonics
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1143:The Paleomap Project
865:Burg, J.-P. (2017).
761:10.1029/2005GC001090
340:Pacific Ring of Fire
1790:Section restoration
1666:Rock microstructure
1328:Convergent boundary
1228:Strain partitioning
1213:Overburden pressure
1203:Mohr–Coulomb theory
797:2011MarPG..28.1123B
752:2006GGG.....7.4016S
696:2002TeNov..14...80A
631:Anderson, Robert S.
595:Planetary Tectonics
452:Planetary tectonics
309:sea-floor spreading
133:economic geologists
47:Tectonics (journal)
1767:Kinematic analysis
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1338:Divergent boundary
1303:Accretionary wedge
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397:neotectonic period
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1661:Pressure solution
1656:Oblique foliation
1536:Exfoliation joint
1526:Columnar jointing
1186:Underlying theory
1050:978-3-540-24181-2
980:978-0-08-102909-1
938:978-1-4020-1903-6
895:10.1111/TER.12662
525:Harper, Douglas.
460:and their moons.
110:mountain-building
39:Tecktonik (dance)
16:(Redirected from
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301:asthenosphere
298:
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233:Carrizo Plain
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78:Ancient Greek
75:
74:
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1604:Thrust fault
1294:
1293:Large-scale
1264:Inclinometer
1238:Stress field
1120:. Retrieved
1116:the original
1100:
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1005:
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873:. Retrieved
860:
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553:
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541:
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447:
440:of an area.
430:
416:
400:
396:
378:
375:Neotectonics
369:Neotectonics
360:
286:
254:thrust fault
243:
211:
198:is present.
169:
141:ore deposits
137:fossil fuels
130:
107:
91:
88:
81:
69:
61:
60:
51:
1785:Paleostress
1671:Slickenside
1646:Crenulation
1599:Fault trace
1594:Fault scarp
1584:Disturbance
1569:Cataclasite
1458:Rift valley
1378:Half-graben
1348:Fault block
1333:Décollement
501:Volcanology
332:earthquakes
289:lithosphere
172:lithosphere
147:to explain
76:; from
18:Geotectonic
1813:Pure shear
1800:Shear zone
1757:Competence
1641:Compaction
1518:Fracturing
1313:Autochthon
1308:Allochthon
1122:31 October
986:23 October
680:Terra Nova
527:"tectonic"
512:References
491:Seismology
385:geological
321:subduction
317:convergent
122:earthquake
92:tektonikós
85:τεκτονικός
72:tectonicus
64:(from
1857:Tectonics
1749:Boudinage
1729:Monocline
1724:Homocline
1704:Anticline
1686:Tectonite
1676:Stylolite
1651:Fissility
1628:lineation
1624:Foliation
1488:Syneclise
1433:Obduction
1403:Inversion
1295:tectonics
770:129068818
700:CiteSeerX
690:: 80–86,
669:Barka, A.
547:tectonics
363:rock salt
336:volcanoes
313:transform
305:divergent
62:Tectonics
1851:Category
1836:Category
1808:Mylonite
1739:Vergence
1734:Syncline
1636:Cleavage
1561:Faulting
722:49553634
671:(2002),
652:23 March
618:craters.
611:23 March
570:23 March
464:See also
330:> 7)
262:foreland
99:building
1709:Chevron
1696:Folding
1541:Fissure
1493:Terrane
1438:Orogeny
1418:Mélange
1353:Fenster
1243:Tension
793:Bibcode
748:Bibcode
692:Bibcode
458:planets
231:on the
114:cratons
1483:Suture
1468:Saddle
1408:Klippe
1373:Graben
1233:Stress
1223:Strain
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433:faults
297:mantle
118:plates
1818:Shear
1546:Joint
1428:Nappe
1388:Horst
1383:Horse
870:(PDF)
766:S2CID
718:S2CID
686:(2),
676:(PDF)
293:crust
291:(the
186:, in
176:rifts
80:
68:
66:Latin
45:, or
1719:Dome
1626:and
1551:Vein
1531:Dike
1463:Rift
1274:Rake
1124:2008
1106:ISBN
1089:ISBN
1075:ISBN
1045:ISBN
1010:ISBN
988:2023
975:ISBN
934:ISBN
877:2022
846:ISBN
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654:2023
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387:and
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