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418:Мичев (Michev), Николай (Nikolay); Михайлов (Mihaylov), Цветко (Tsvetko); Вапцаров (Vaptsarov), Иван (Ivan); Кираджиев (Kiradzhiev), Светлин (Svetlin) (1980).
375:
Péron-Pinvidic, Gwenn; Manatschal, Gianreto (2010). "From microcontinents to extensional allochthons: witnesses of how continents rift and break apart?".
499:
Monroe, James S., and Reed
Wicander. The Changing Earth: Exploring Geology and Evolution. 2nd educational Belmont: Wadsworth Publishing Company, 1997.
548:
446:
118:, hills, ridges, lakes, valleys, etc.) are sometimes formed when the faults have a large vertical displacement. Adjacent raised blocks (
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130:. Often the movement of these blocks is accompanied by tilting, due to compaction or stretching of the crust at that point.
17:
791:
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473:
348:
A crustal block may or may not also comprise a tectonostratigraphic terrane that has a specific geologic definition.
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block mountains have one gently sloping side and one steep side with an exposed scarp, and are common in the
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is a smaller example. There are two main types of block mountains; uplifted blocks between two faults and
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Lifted type block mountains have two steep sides exposing both sides scarps, leading to the
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114:. However vertical movement of blocks produces much more dramatic results. Landforms (
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microcontinents, continental ribbons, H-blocks, extensional allochthons and outer highs.
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are very large blocks of rock, sometimes hundreds of kilometres in extent, created by
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110:, most motion between blocks is horizontal, that is parallel to the Earth's crust by
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460:Дончев (Donchev), Дончо (Doncho); Каракашев (Karakashev), Христо (Hristo) (2004).
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Large blocks of rock created by tectonic and localized stresses in Earth's crust
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426:] (in Bulgarian). Sofia: Наука и култура (Nauka i kultura). p. 368.
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30:"Fault-block" redirects here. For geological faulting in general, see
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are called microplates. Continent-sized blocks are called variously
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92:. Large crustal blocks broken off from tectonic plates are called
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Because most stresses relate to the tectonic activity of moving
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462:Теми по физическа и социално-икономическа география на България
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219:
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Topics on
Physical and Social-Economic Geography of Bulgaria
65:
Horizontal movement between blocks along a strike-slip fault
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468:] (in Bulgarian). Sofia: Ciela. pp. 128–129.
80:. Large areas of bedrock are broken up into blocks by
355:
Paleomagnetism: Magnetic
Domains to Geologic Terranes
96:. Those terranes which are the full thickness of the
492:
Plummer, Charles, David McGeary, and Diane
Carlson.
437:Димитрова (Dimitrova), Людмила (Lyudmila) (2004).
449:, Bulgarian Foundation "Biodiversity". p. 53.
84:. Blocks are characterized by relatively uniform
459:
357:Blackwell, pp. 205–223, page 205, archived
1227:
436:
352:"Chapter 11: Applications to Regional Tectonics"
88:. The largest of these fault blocks are called
542:
439:Национален парк "Пирин". План за управление
549:
535:
430:
214:valley, a graben between two horsts - the
445:] (in Bulgarian). и колектив. Sofia:
330: – The formation of mountain ranges
167:Fault-block mountains often result from
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147:
133:
60:
36:
175:. These can be small or form extensive
14:
1228:
556:
530:
443:Pirin National Park. Management Plan
160:Tilted fault-block formation in the
792:List of tectonic plate interactions
24:
496:8th ed. McGraw-Hill, Boston, 1999.
25:
1252:
511:
447:Ministry of Environment and Water
424:Geographic Dictionary of Bulgaria
261:(vaulted domed shaped horst) and
206:terrain seen in various parts of
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195:mainly controlled by one fault.
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368:
341:
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1:
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420:Географски речник на България
269:situated between the complex
249:, including the well defined
57:) visible from right to left.
265:- a horst forming a massive
7:
321:
122:) and down-dropped blocks (
10:
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152:Lifted fault-block geology
137:
76:and localized stresses in
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877:Thick-skinned deformation
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350:Bulter, Robert F. (1992)
882:Thin-skinned deformation
658:Stereographic projection
461:
438:
419:
334:
648:Orthographic projection
631:Measurement conventions
577:Lamé's stress ellipsoid
397:10.1144/1354-079309-903
1236:Mountain geomorphology
291:region of the western
164:
153:
140:List of mountain types
66:
58:
1159:Paleostress inversion
852:Strike-slip tectonics
722:Extensional tectonics
702:Continental collision
572:Deformation mechanism
518:Fault-Block Mountains
179:systems, such as the
173:extensional tectonics
159:
151:
134:Fault-block mountains
64:
40:
737:Fold and thrust belt
377:Petroleum Geoscience
302:is the basin of the
53:range); upfaulting (
18:Fault-block mountain
1169:Section restoration
1045:Rock microstructure
707:Convergent boundary
607:Strain partitioning
592:Overburden pressure
582:Mohr–Coulomb theory
389:2010PetGe..16..189P
1241:Structural geology
1146:Kinematic analysis
802:Mountain formation
717:Divergent boundary
682:Accretionary wedge
558:Structural geology
365:on 26 October 2004
171:, an indicator of
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154:
112:strike-slip faults
67:
59:
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1154:3D fold evolution
1040:Pressure solution
1035:Oblique foliation
915:Exfoliation joint
905:Columnar jointing
565:Underlying theory
507:(pp. 234,-8)
181:East African Rift
144:Mountain building
16:(Redirected from
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958:Detachment fault
953:Cataclastic rock
887:Thrust tectonics
857:Structural basin
832:Pull-apart basin
772:Horst and graben
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494:Physical Geology
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363:Internet Archive
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298:An example of a
257:(linear horst),
247:Southeast Europe
230:), and also the
216:Vosges mountains
126:) can form high
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512:External links
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304:Narmada River
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293:United States
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259:Rila mountain
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43:Hanging Hills
39:
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983:Thrust fault
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672:Large-scale
643:Inclinometer
617:Stress field
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277:and that of
224:Black Forest
197:
185:Death Valley
166:
105:
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70:Fault blocks
69:
68:
1164:Paleostress
1050:Slickenside
1025:Crenulation
978:Fault trace
973:Fault scarp
963:Disturbance
948:Cataclasite
837:Rift valley
757:Half-graben
727:Fault block
712:Décollement
285:Tilted type
273:valleys of
212:Upper Rhine
177:rift valley
162:Teton Range
128:escarpments
98:lithosphere
47:Connecticut
1230:Categories
1192:Pure shear
1179:Shear zone
1136:Competence
1020:Compaction
897:Fracturing
692:Autochthon
687:Allochthon
487:References
383:(3): 189.
222:) and the
189:California
138:See also:
1128:Boudinage
1108:Monocline
1103:Homocline
1083:Anticline
1065:Tectonite
1055:Stylolite
1030:Fissility
1007:lineation
1003:Foliation
867:Syneclise
812:Obduction
782:Inversion
674:tectonics
405:131142997
267:anticline
255:Belasitsa
116:mountains
86:lithology
1215:Category
1187:Mylonite
1118:Vergence
1113:Syncline
1015:Cleavage
940:Faulting
322:See also
318:horsts.
243:Bulgaria
94:terranes
74:tectonic
1088:Chevron
1075:Folding
920:Fissure
872:Terrane
817:Orogeny
797:Mélange
732:Fenster
622:Tension
385:Bibcode
328:Orogeny
316:Satpura
312:Vindhya
236:Rhodope
228:Germany
169:rifting
124:grabens
862:Suture
847:Saddle
787:Klippe
752:Graben
612:Stress
602:Strain
503:
472:
403:
300:graben
275:Struma
271:graben
251:horsts
239:Massif
220:France
208:Europe
204:graben
183:zone.
120:horsts
108:plates
82:faults
1197:Shear
925:Joint
807:Nappe
767:Horst
762:Horse
464:[
441:[
422:[
401:S2CID
335:Notes
308:India
279:Mesta
200:horst
55:horst
1098:Dome
1005:and
930:Vein
910:Dike
842:Rift
653:Rake
501:ISBN
470:ISBN
359:here
314:and
232:Rila
226:(in
218:(in
202:and
142:and
41:The
393:doi
361:by
306:in
253:of
241:in
187:in
45:of
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520:—
399:.
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381:16
379:.
295:.
281:.
245:,
234:-
550:e
543:t
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407:.
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49:(
34:.
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
