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
323:
Shiner, P (2004). "Thin-skinned versus thick-skinned structural models for
Apulian carbonate reservoirs: constraints from the Val d'Agri Fields, S Apennines, Italy".
151:
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
511:
290:
Butler, R.; Bond, C. (2020). "Chapter 9 - Thrust systems and contractional tectonics". In
Scarselli, N.; Adam, J.; Chiarella, D. (eds.).
485:
Contraction: Chapter 16; A complementary resource to
Chapter 16 of the textbook "Strukturgeologi" by Haakon Fossen & Roy Gabrielsen
470:
Marton, G, & Schoenborn, G. 2008. Salt
Tectonics of the Continent-Ocean Transition, Deep-Water Angola. MAPG conference abstract
419:
754:
469:
17:
307:
253:, the extensional faulting that forms at the landward side will be balanced at the front of the wedge by a series of
504:
361:
539:
325:
388:"Applying thick-skinned tectonic models to the Apennine thrust belt of ItalyâLimitations and implications"
1198:
1177:
497:
195:
387:
457:
839:
143:
109:
215:
844:
620:
484:
120:
105:
35:
1108:
127:
developed in the foreland of a collisional zone. This is particularly the case where a good basal
610:
544:
445:
434:
1121:
925:
814:
684:
664:
564:
534:
123:
refers to shortening that only involves the sedimentary cover. This style is typical of many
85:
65:
61:
1098:
982:
699:
654:
334:
124:
8:
1131:
1007:
992:
969:
965:
744:
669:
569:
554:
172:
155:
73:
338:
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
1203:
1080:
977:
859:
764:
679:
644:
574:
520:
299:
227:
77:
150:
rather than just the overlying cover. This type of geometry is typically found in the
1116:
1050:
1002:
997:
877:
867:
809:
584:
415:
303:
223:
180:
346:
920:
915:
824:
819:
794:
734:
694:
549:
342:
295:
245:. This wedge of material will tend to spread under gravity and, where an effective
1159:
1055:
955:
930:
902:
887:
789:
739:
729:
724:
600:
409:
242:
183:
81:
69:
53:
1060:
1037:
1022:
892:
872:
784:
709:
704:
659:
625:
615:
559:
270:
250:
238:
191:
89:
674:
1192:
950:
219:
187:
176:
147:
30:
945:
605:
579:
161:
101:
1126:
1012:
987:
940:
935:
910:
799:
719:
689:
258:
246:
128:
60:. It is one of the three main types of tectonic regime, the others being
57:
1154:
1141:
649:
199:
759:
1090:
1070:
1065:
1045:
1027:
1017:
829:
774:
636:
489:
132:
49:
1149:
1075:
262:
171:
The most significant areas of thrust tectonics are associated with
407:
882:
834:
779:
52:
processes associated with, the shortening and thickening of the
749:
714:
266:
203:
385:
769:
411:
Geology and
Geophysics of an Arc-continent Collision, Taiwan
804:
209:
395:
Thrust tectonics and hydrocarbon systems: AAPG Memoir 82
162:
Geological environments associated with thrust tectonics
283:
414:. Special Paper 358. Geological Society of America.
48:
is concerned with the structures formed by, and the
1190:
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:
505:
408:Timothy Briggs Byrne; Char-Shine Liu (2002).
257:. Examples include the outboard part of the
198:) and collisions between a continent and an
138:
115:
512:
498:
289:
29:
359:
210:Restraining bends on strike-slip faults
135:or a zone of high pore fluid pressure.
14:
1191:
519:
322:
493:
95:
166:
755:List of tectonic plate interactions
146:refers to shortening that involves
24:
300:10.1016/B978-0-444-64134-2.00008-0
233:
25:
1215:
478:
369:AAPG Search and Discovery Article
68:. These match the three types of
1173:
1172:
347:10.1016/j.marpetgeo.2003.11.020
292:Principles of Geologic Analysis
463:
451:
439:
428:
401:
379:
353:
316:
13:
1:
276:
27:Concept in structural geology
326:Marine and Petroleum Geology
175:leading to the formation of
173:destructive plate boundaries
7:
196:Zagros fold and thrust belt
10:
1220:
202:such as that which formed
1168:
1140:
1107:
1089:
1036:
964:
901:
858:
840:Thick-skinned deformation
634:
593:
527:
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 thickening
1186:
1185:
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
1211:
1176:
1175:
921:Detachment fault
916:Cataclastic rock
850:Thrust tectonics
820:Structural basin
795:Pull-apart basin
735:Horst and graben
514:
507:
500:
491:
490:
472:
467:
461:
455:
449:
443:
437:
432:
426:
425:
405:
399:
398:
392:
383:
377:
376:
366:
357:
351:
350:
320:
314:
313:
287:
243:spreading centre
42:Thrust tectonics
21:
1219:
1218:
1214:
1213:
1212:
1210:
1209:
1208:
1189:
1188:
1187:
1182:
1164:
1136:
1103:
1085:
1056:Detachment fold
1032:
960:
956:Transform fault
931:Fault mechanics
897:
854:
790:Plate tectonics
740:Intra-arc basin
630:
601:Brunton compass
589:
523:
518:
481:
476:
475:
468:
464:
456:
452:
444:
440:
433:
429:
422:
406:
402:
390:
384:
380:
364:
358:
354:
321:
317:
310:
288:
284:
279:
271:salt detachment
269:margin (with a
239:Passive margins
236:
234:Passive margins
212:
184:tectonic plates
169:
164:
141:
131:exists such as
118:
98:
90:passive margins
28:
23:
22:
15:
12:
11:
5:
1217:
1207:
1206:
1201:
1184:
1183:
1181:
1180:
1169:
1166:
1165:
1163:
1162:
1157:
1152:
1146:
1144:
1138:
1137:
1135:
1134:
1129:
1124:
1119:
1113:
1111:
1105:
1104:
1102:
1101:
1095:
1093:
1087:
1086:
1084:
1083:
1078:
1073:
1068:
1063:
1058:
1053:
1048:
1042:
1040:
1034:
1033:
1031:
1030:
1025:
1023:Tectonic phase
1020:
1015:
1010:
1005:
1000:
995:
990:
985:
980:
974:
972:
962:
961:
959:
958:
953:
948:
943:
938:
933:
928:
923:
918:
913:
907:
905:
899:
898:
896:
895:
890:
885:
880:
875:
870:
864:
862:
856:
855:
853:
852:
847:
842:
837:
832:
827:
822:
817:
812:
807:
802:
797:
792:
787:
785:Passive margin
782:
777:
772:
767:
762:
757:
752:
747:
742:
737:
732:
727:
722:
717:
712:
710:Foreland basin
707:
705:Fold mountains
702:
697:
692:
687:
682:
677:
672:
667:
662:
660:Back-arc basin
657:
652:
647:
641:
639:
632:
631:
629:
628:
626:Strike and dip
623:
618:
613:
608:
603:
597:
595:
591:
590:
588:
587:
582:
577:
572:
567:
562:
560:Rock mechanics
557:
552:
547:
542:
537:
531:
529:
525:
524:
517:
516:
509:
502:
494:
488:
487:
480:
479:External links
477:
474:
473:
462:
450:
438:
427:
420:
400:
378:
352:
333:(7): 805â827.
315:
308:
281:
280:
278:
275:
235:
232:
211:
208:
192:Eurasian Plate
177:orogenic belts
168:
165:
163:
160:
148:basement rocks
140:
137:
117:
114:
97:
94:
70:plate boundary
26:
9:
6:
4:
3:
2:
1216:
1205:
1202:
1200:
1197:
1196:
1194:
1179:
1171:
1170:
1167:
1161:
1158:
1156:
1153:
1151:
1148:
1147:
1145:
1143:
1139:
1133:
1130:
1128:
1125:
1123:
1120:
1118:
1115:
1114:
1112:
1110:
1106:
1100:
1097:
1096:
1094:
1092:
1088:
1082:
1079:
1077:
1074:
1072:
1069:
1067:
1064:
1062:
1059:
1057:
1054:
1052:
1049:
1047:
1044:
1043:
1041:
1039:
1035:
1029:
1026:
1024:
1021:
1019:
1016:
1014:
1011:
1009:
1006:
1004:
1001:
999:
996:
994:
991:
989:
986:
984:
981:
979:
976:
975:
973:
971:
967:
963:
957:
954:
952:
951:Transfer zone
949:
947:
944:
942:
939:
937:
934:
932:
929:
927:
924:
922:
919:
917:
914:
912:
909:
908:
906:
904:
900:
894:
891:
889:
886:
884:
881:
879:
876:
874:
871:
869:
866:
865:
863:
861:
857:
851:
848:
846:
843:
841:
838:
836:
833:
831:
828:
826:
823:
821:
818:
816:
813:
811:
808:
806:
803:
801:
798:
796:
793:
791:
788:
786:
783:
781:
778:
776:
773:
771:
768:
766:
763:
761:
758:
756:
753:
751:
748:
746:
743:
741:
738:
736:
733:
731:
728:
726:
723:
721:
718:
716:
713:
711:
708:
706:
703:
701:
698:
696:
693:
691:
688:
686:
683:
681:
678:
676:
673:
671:
668:
666:
663:
661:
658:
656:
653:
651:
648:
646:
643:
642:
640:
638:
633:
627:
624:
622:
619:
617:
614:
612:
609:
607:
604:
602:
599:
598:
596:
592:
586:
583:
581:
578:
576:
573:
571:
568:
566:
563:
561:
558:
556:
553:
551:
550:Mohr's circle
548:
546:
543:
541:
538:
536:
533:
532:
530:
526:
522:
515:
510:
508:
503:
501:
496:
495:
492:
486:
483:
482:
471:
466:
460:
454:
448:
442:
436:
431:
423:
417:
413:
412:
404:
396:
389:
382:
374:
370:
363:
356:
348:
344:
340:
336:
332:
328:
327:
319:
311:
309:9780444641359
305:
301:
297:
293:
286:
282:
274:
272:
268:
264:
260:
256:
252:
248:
244:
240:
231:
229:
225:
221:
220:transpression
217:
207:
205:
201:
197:
193:
189:
188:Arabian Plate
185:
182:
178:
174:
159:
157:
153:
149:
145:
136:
134:
130:
126:
122:
113:
111:
107:
103:
93:
91:
87:
83:
79:
75:
71:
67:
63:
59:
55:
51:
47:
43:
37:
32:
19:
946:Thrust fault
849:
635:Large-scale
606:Inclinometer
580:Stress field
465:
453:
441:
430:
410:
403:
394:
381:
372:
368:
355:
330:
324:
318:
291:
285:
254:
237:
213:
170:
142:
119:
100:In areas of
99:
45:
41:
40:
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
1195::
393:.
371:.
367:.
341:.
331:21
329:.
302:.
230:.
206:.
158:.
92:.
72:,
513:e
506:t
499:v
424:.
375:.
349:.
345::
337::
312:.
298::
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.