31:
1174:
446:
Gomez, F., Nemer, T., Tabet, C., Meghraoui, M. & Barazangi, M. 2007. Strain partitioning of active transpression within the
Lebanese restraining bend of the Dead Sea Fault (Lebanon and SW Syria). Geological Society, London, Special Publications; 290;
84:(strike-slip). There are two main types of thrust tectonics, thin-skinned and thick-skinned, depending on whether or not basement rocks are involved in the deformation. The principle geological environments where thrust tectonics is observed are zones of
458:
Bilotti, F. & Shaw, J.H. 2005. Deep-water Niger Delta fold and thrust belt modeled as a critical taper wedge: The influence of elevated basal fluid pressure on structural styles. AAPG Bulletin; 89; 11;
435:
Rust, D. 1998. Contractional and extensional structures in the transpressive âBig Bendâ of the San
Andreas fault, southern California. Geological Society, London, Special Publications; 135; pp. 119â126
362:"Confirmation of Thin-skinned Thrust Faulting in Foreland Fold-Thrust Belts and Its Impact on Hydrocarbon Exploration: Bally, Gordy, and Stewart, Bulletin of Canadian Petroleum Geology, 1966"
218:
is offset along strike such that the resulting bend in the fault hinders easy movement, e.g. a right stepping bend on a sinistral (left-lateral) fault, this will cause local shortening or
386:
Butler, R. W. H.; Mazzoli, S.; Corrado, S.; De
Donatis, M.; Di Bucci, D.; Gambini, R.; Naso, G.; Nicolai, C.; Scrocca, D.; Shiner, P.; Zucconi, V. (2004). McClay, K. R. (ed.).
154:
of a collisional zone. This style may also occur in the foreland where no effective decollement surface is present or where pre-existing extensional rift structures may be
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Shiner, P (2004). "Thin-skinned versus thick-skinned structural models for
Apulian carbonate reservoirs: constraints from the Val d'Agri Fields, S Apennines, Italy".
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112:. The distinction is important as attempts to structurally restore the deformation will give very different results depending on the assumed geometry.
241:
are characterised by large prisms of sedimentary material deposited since the original break-up of a continent associated with formation of a new
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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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Contraction: Chapter 16; A complementary resource to
Chapter 16 of the textbook "Strukturgeologi" by Haakon Fossen & Roy Gabrielsen
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Marton, G, & Schoenborn, G. 2008. Salt
Tectonics of the Continent-Ocean Transition, Deep-Water Angola. MAPG conference abstract
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253:, the extensional faulting that forms at the landward side will be balanced at the front of the wedge by a series of
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388:"Applying thick-skinned tectonic models to the Apennine thrust belt of ItalyâLimitations and implications"
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developed in the foreland of a collisional zone. This is particularly the case where a good basal
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refers to shortening that only involves the sedimentary cover. This style is typical of many
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294:. Regional Geology and Tectonics. Vol. 1 (2 ed.). Elsevier. pp. 149â167.
88:, restraining bends on strike-slip faults and as part of detached fault systems on some
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rather than just the overlying cover. This type of geometry is typically found in the
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245:. This wedge of material will tend to spread under gravity and, where an effective
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60:. It is one of the three main types of tectonic regime, the others being
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The most significant areas of thrust tectonics are associated with
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processes associated with, the shortening and thickening of the
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Geology and
Geophysics of an Arc-continent Collision, Taiwan
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Thrust tectonics and hydrocarbon systems: AAPG Memoir 82
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Geological environments associated with thrust tectonics
414:. Special Paper 358. Geological Society of America.
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is concerned with the structures formed by, and the
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222:. Examples include the 'Big Bend' region of the
179:. The two main types are: the collision of two
34:Cross-section diagram of the frontal part of a
104:tectonics, two main processes are recognized:
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408:Timothy Briggs Byrne; Char-Shine Liu (2002).
8:
257:. Examples include the outboard part of the
198:) and collisions between a continent and an
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498:
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210:Restraining bends on strike-slip faults
135:or a zone of high pore fluid pressure.
7:
755:List of tectonic plate interactions
146:refers to shortening that involves
300:10.1016/B978-0-444-64134-2.00008-0
25:
369:AAPG Search and Discovery Article
68:. These match the three types of
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347:10.1016/j.marpetgeo.2003.11.020
292:Principles of Geologic Analysis
1:
27:Concept in structural geology
326:Marine and Petroleum Geology
175:leading to the formation of
173:destructive plate boundaries
196:Zagros fold and thrust belt
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202:such as that which formed
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840:Thick-skinned deformation
249:layer is present such as
144:Thick-skinned deformation
139:Thick-skinned deformation
110:thick-skinned deformation
845:Thin-skinned deformation
621:Stereographic projection
121:Thin-skinned deformation
116:Thin-skinned deformation
106:thin-skinned deformation
36:thin-skinned thrust zone
611:Orthographic projection
594:Measurement conventions
540:Lamé's stress ellipsoid
360:Hatcher, R. D. (2007).
261:(with an overpressured
46:contractional tectonics
38:
1122:Paleostress inversion
815:Strike-slip tectonics
685:Extensional tectonics
665:Continental collision
535:Deformation mechanism
125:fold and thrust belts
86:continental collision
66:strike-slip tectonics
62:extensional tectonics
33:
700:Fold and thrust belt
265:detachment) and the
1132:Section restoration
1008:Rock microstructure
670:Convergent boundary
570:Strain partitioning
555:Overburden pressure
545:MohrâCoulomb theory
339:2004MarPG..21..805S
226:, and parts of the
194:, which formed the
1199:Structural geology
1109:Kinematic analysis
765:Mountain formation
680:Divergent boundary
645:Accretionary wedge
521:Structural geology
397:. pp. 647â67.
228:Dead Sea Transform
96:Deformation styles
80:(extensional) and
39:
18:Crustal shortening
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1117:3D fold evolution
1003:Pressure solution
998:Oblique foliation
878:Exfoliation joint
868:Columnar jointing
528:Underlying theory
421:978-0-8137-2358-7
224:San Andreas Fault
216:strike-slip fault
186:(for example the
167:Collisional zones
16:(Redirected from
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850:Thrust tectonics
820:Structural basin
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606:Inclinometer
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100:In areas of
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1127:Paleostress
1013:Slickenside
988:Crenulation
941:Fault trace
936:Fault scarp
926:Disturbance
911:Cataclasite
800:Rift valley
720:Half-graben
690:Fault block
675:DĂ©collement
259:Niger delta
255:toe-thrusts
181:continental
129:decollement
58:lithosphere
1193:Categories
1155:Pure shear
1142:Shear zone
1099:Competence
983:Compaction
860:Fracturing
655:Autochthon
650:Allochthon
277:References
247:detachment
200:island arc
152:hinterland
76:(thrust),
74:convergent
1204:Tectonics
1091:Boudinage
1071:Monocline
1066:Homocline
1046:Anticline
1028:Tectonite
1018:Stylolite
993:Fissility
970:lineation
966:Foliation
830:Syneclise
775:Obduction
745:Inversion
637:tectonics
459:1475â1491
82:transform
78:divergent
1178:Category
1150:Mylonite
1081:Vergence
1076:Syncline
978:Cleavage
903:Faulting
263:mudstone
156:inverted
50:tectonic
1051:Chevron
1038:Folding
883:Fissure
835:Terrane
780:Orogeny
760:MĂ©lange
695:Fenster
585:Tension
447:285â303
335:Bibcode
214:When a
825:Suture
810:Saddle
750:Klippe
715:Graben
575:Stress
565:Strain
418:
306:
267:Angola
204:Taiwan
102:thrust
1160:Shear
888:Joint
770:Nappe
730:Horst
725:Horse
391:(PDF)
373:70034
365:(PDF)
54:crust
1061:Dome
968:and
893:Vein
873:Dike
805:Rift
616:Rake
416:ISBN
304:ISBN
251:salt
190:and
133:salt
108:and
64:and
343:doi
296:doi
273:).
56:or
44:or
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