34:
41:
57:
73:
89:
33:
104:
557:
206:
moving southwest) albeit one suggest the opposite (subducted plate moving to the northeast). In the
Cambrian the Timanide Orogen is believed to have developed in a
393:"Pre-Ordovician tectonic evolution and volcano-plutonic associations of the Timanides and northern Pre-Uralides, northeast part of the East European Craton"
363:"The Timanide, Caledonide and Uralide orogens in the Eurasian high Arctic, and relationships to the palaeo-continents Laurentia, Baltica and Siberia"
214:
collided between 528 and 510 million years ago. Some researchers do however dissent from this view suggesting there was never such a collision.
236:. Studies of sediments points that it is likely that the erosion of the orogen was beginning in the Cambrian and then became stronger in
1123:
172:
that has an oblique disposition. The northeastern parts of the orogen are made up of volcanic and sedimentary rocks, granitoids and few
346:
Roberts, D.; Olovyanishnikov, V. (2004). "Structural and tectonic development of the
Timanide orogen". In Gee, D.G.; Pease, V. (eds.).
288:
Another name for the orogen is "Baikalides" which is a name that has been used in wider sense to refer chiefly to orogens south of the
991:
320:
Gee, D.G.; Pease, V. (2004). "The
Neoproterozoic Timanide Ororgen of eastern Baltica: introduction". In Gee, D.G.; Pease, V. (eds.).
1133:
543:
1138:
1118:
1072:
550:
168:
of the orogen. To the west, at the
Varanger Peninsula, the north-west oriented Timanide Orogen is truncated by the younger
682:
657:
632:
1143:
1103:
1148:
496:
Kuznetsov, N.B. (2008). "The
Cambrian Pre-Uralide–Timanide Orogen: Structural Evidence for Its Collisional Origin".
1128:
1113:
1047:
1001:
795:
607:
1021:
775:
1153:
1057:
1158:
952:
897:
617:
612:
1067:
1006:
942:
627:
225:
444:"Age Constraints for the Pre–Uralide–Timanide Orogenic Event Inferred from the Study of Detrital Zircons"
1082:
1026:
962:
207:
229:
1108:
1062:
800:
708:
505:
455:
406:
947:
790:
1042:
723:
602:
248:
144:
in the
Timanide orogeny. The orogen is about 3000 km long. Its extreme points include the southern
866:
770:
202:
that existed to the northeast of it. Most studies interpret subduction as going inward (subducted
742:
521:
471:
157:
47:
871:
836:
831:
760:
397:
63:
329:
1016:
927:
513:
463:
414:
321:
177:
122:
902:
677:
293:
289:
153:
130:
79:
986:
780:
672:
391:
Kuznetsov, N.N; Soboleva, A.A.; Udoratina, O.V; Hertseva, M.V.; Andreichev, V.L. (2007).
509:
459:
410:
856:
821:
785:
765:
597:
587:
244:
203:
141:
1097:
1052:
1011:
841:
826:
713:
692:
667:
662:
592:
582:
566:
525:
475:
443:
442:
Orlov, S.Yu.; Kuznetsov, N.B.; Miller, E.D.; Soboleva, A.A.; Udoratina, O.V. (2011).
392:
362:
322:
188:
977:
574:
996:
937:
912:
861:
851:
687:
252:
233:
169:
161:
149:
95:
17:
957:
907:
752:
728:
622:
517:
467:
237:
199:
418:
271:
All coordinates in this article are in relation to present-day geography and
876:
184:
173:
165:
881:
535:
221:
195:
296:, was for long time the most common term for the orogen until the 1990s.
922:
917:
846:
718:
649:
276:
217:
211:
181:
176:. In contrast the southwestern part of the orogen is made up mostly of
137:
109:
932:
816:
133:
292:. Among Russian scientists the term "Baikalian", coined in 1935 by
145:
539:
369:. Geological Society, London, Memoirs. pp. 507–520
255:
compiled the existing knowledge on the orogen in 1900.
350:. Geological Society, London, Memoirs. pp. 47–57.
348:
324:
1035:
975:
890:
809:
750:
741:
701:
648:
641:
573:
251:who published works in 1899 and 1901 respectively.
129:, literally: "Protouralian–Timanide Orogen") is a
361:Gee, D.G.; Bogolepova, O.K.; Lorenz, H. (2006).
328:. Geological Society, London, Memoirs. pp.
437:
435:
243:The first geologists to study the orogen where
551:
386:
384:
341:
339:
8:
27:Orogen that formed during the Neoproterozoic
315:
313:
747:
645:
558:
544:
536:
40:
365:. In Gee, D.G.; Stephenson, R.A. (eds.).
56:
198:the Timanide Orogen was associated to a
309:
275:to the past disposition of continents,
264:
72:
220:of the Timanide Orogen have produced
7:
194:From the Late Neoproterozoic o the
88:
25:
87:
71:
55:
39:
32:
992:Central Skåne Volcanic Province
1073:Transscandinavian Igneous Belt
170:Scandinavian Caledonide Orogen
1:
367:European Lithosphere Dynamics
160:peninsulas in the north. The
136:that formed in northeastern
1175:
1124:Geology of European Russia
1048:Blekinge-Bornholm Province
1002:Kattsund-Koster dyke swarm
658:Billingen terminal moraine
224:that are now found in the
191:are common in the orogen.
127:Ороген Протоуралид-Тиманид
796:Sorgenfrei-Tornquist Zone
776:Nordfjord-Sogn Detachment
633:Sub-Mesozoic hilly relief
518:10.1134/S1028334X08090122
468:10.1134/S1028334X11090078
228:, including the Cambrian
126:
1134:Neoproterozoic orogenies
1058:Scandinavian Caledonides
801:South Finland Shear Zone
719:Jotnian sedimentary rock
419:10.1016/j.gr.2006.10.021
1068:Sveconorwegian Province
898:Central Swedish lowland
683:Skövde terminal moraine
608:South Småland peneplain
567:Geology of Fennoscandia
210:context as Baltica and
112:of the Timanide Orogen.
1022:Särna Alkaline Complex
1007:Kola Alkaline Province
943:Scandinavian Mountains
628:Sub-Cambrian peneplain
498:Doklady Earth Sciences
448:Doklady Earth Sciences
226:East European Platform
1139:Neoproterozoic Europe
1119:Geology of Kazakhstan
1083:Western Gneiss Region
1063:Svecofennian Province
1036:Provinces and orogens
1027:Satakunta dyke swarms
963:White Sea Rift System
249:Feodosy Tschernyschev
208:continental collision
148:in the south and the
903:Gulf of Bothnia rift
810:Large impact craters
709:Alum Shale Formation
105:class=notpageimage|
1144:Ediacaran orogenies
1104:Orogenies of Europe
1043:Belomorian Province
603:Ostrobothnian Plain
510:2008DokES.423.1383K
460:2011DokES.440.1216O
411:2007GondR..12..305K
1149:Cambrian orogenies
953:South Swedish Dome
913:Lake Ladoga graben
48:Varanger Peninsula
1129:Geology of Russia
1114:Geology of Norway
1091:
1090:
1017:Rapakivi granites
971:
970:
908:Lake Inari graben
832:Hummeln structure
737:
736:
642:Sedimentary cover
398:Gondwana Research
230:Sablino Formation
178:sedimentary rocks
64:Rybachy Peninsula
16:(Redirected from
1166:
928:Norrland terrain
748:
724:Reusch's Moraine
702:Sedimentary rock
646:
560:
553:
546:
537:
530:
529:
504:(9): 1383–1387.
493:
487:
486:
484:
482:
454:(1): 1216–1221.
439:
430:
429:
427:
425:
388:
379:
378:
376:
374:
358:
352:
351:
343:
334:
333:
327:
317:
297:
286:
280:
269:
128:
91:
90:
75:
74:
59:
58:
43:
42:
36:
21:
18:Timanide orogeny
1174:
1173:
1169:
1168:
1167:
1165:
1164:
1163:
1154:Cambrian Europe
1094:
1093:
1092:
1087:
1078:Timanide Orogen
1031:
967:
891:Morphostrucures
886:
805:
733:
697:
678:Sevetti moraine
637:
618:200 m peneplain
613:300 m peneplain
569:
564:
534:
533:
495:
494:
490:
480:
478:
441:
440:
433:
423:
421:
390:
389:
382:
372:
370:
360:
359:
355:
345:
344:
337:
319:
318:
311:
306:
301:
300:
290:Siberian Craton
287:
283:
270:
266:
261:
200:subduction zone
196:Middle Cambrian
119:Timanide Orogen
115:
114:
113:
107:
101:
100:
99:
98:
92:
84:
83:
82:
80:Kanin Peninsula
76:
68:
67:
66:
60:
52:
51:
50:
44:
28:
23:
22:
15:
12:
11:
5:
1172:
1170:
1162:
1161:
1159:Ural Mountains
1156:
1151:
1146:
1141:
1136:
1131:
1126:
1121:
1116:
1111:
1106:
1096:
1095:
1089:
1088:
1086:
1085:
1080:
1075:
1070:
1065:
1060:
1055:
1050:
1045:
1039:
1037:
1033:
1032:
1030:
1029:
1024:
1019:
1014:
1009:
1004:
999:
994:
989:
983:
981:
973:
972:
969:
968:
966:
965:
960:
958:Vättern graben
955:
950:
948:Scanian horsts
945:
940:
935:
930:
925:
920:
915:
910:
905:
900:
894:
892:
888:
887:
885:
884:
879:
874:
869:
864:
859:
857:Ritland crater
854:
849:
844:
839:
834:
829:
824:
822:Gardnos crater
819:
813:
811:
807:
806:
804:
803:
798:
793:
791:Röjnoret Fault
788:
786:Protogine Zone
783:
778:
773:
768:
766:Iapetus Suture
763:
761:Burträsk Fault
757:
755:
745:
739:
738:
735:
734:
732:
731:
729:Visingsö Group
726:
721:
716:
711:
705:
703:
699:
698:
696:
695:
690:
685:
680:
675:
670:
665:
660:
654:
652:
643:
639:
638:
636:
635:
630:
625:
620:
615:
610:
605:
600:
598:Paleic surface
595:
590:
588:Hardangervidda
585:
579:
577:
571:
570:
565:
563:
562:
555:
548:
540:
532:
531:
488:
431:
405:(3): 305–323.
380:
353:
335:
308:
307:
305:
302:
299:
298:
281:
263:
262:
260:
257:
245:Wilhelm Ramsay
189:volcanic rocks
142:Neoproterozoic
103:
102:
94:
93:
86:
85:
78:
77:
70:
69:
62:
61:
54:
53:
46:
45:
38:
37:
31:
30:
29:
26:
24:
14:
13:
10:
9:
6:
4:
3:
2:
1171:
1160:
1157:
1155:
1152:
1150:
1147:
1145:
1142:
1140:
1137:
1135:
1132:
1130:
1127:
1125:
1122:
1120:
1117:
1115:
1112:
1110:
1107:
1105:
1102:
1101:
1099:
1084:
1081:
1079:
1076:
1074:
1071:
1069:
1066:
1064:
1061:
1059:
1056:
1054:
1053:Kola Province
1051:
1049:
1046:
1044:
1041:
1040:
1038:
1034:
1028:
1025:
1023:
1020:
1018:
1015:
1013:
1010:
1008:
1005:
1003:
1000:
998:
995:
993:
990:
988:
985:
984:
982:
979:
974:
964:
961:
959:
956:
954:
951:
949:
946:
944:
941:
939:
936:
934:
931:
929:
926:
924:
921:
919:
918:Lofoten horst
916:
914:
911:
909:
906:
904:
901:
899:
896:
895:
893:
889:
883:
880:
878:
875:
873:
870:
868:
865:
863:
860:
858:
855:
853:
850:
848:
845:
843:
842:Lockne crater
840:
838:
835:
833:
830:
828:
827:Granby crater
825:
823:
820:
818:
815:
814:
812:
808:
802:
799:
797:
794:
792:
789:
787:
784:
782:
779:
777:
774:
772:
769:
767:
764:
762:
759:
758:
756:
754:
749:
746:
744:
740:
730:
727:
725:
722:
720:
717:
715:
714:Hedmark Group
712:
710:
707:
706:
704:
700:
694:
693:Veiki moraine
691:
689:
686:
684:
681:
679:
676:
674:
671:
669:
668:Rogen moraine
666:
664:
663:Pulju moraine
661:
659:
656:
655:
653:
651:
647:
644:
640:
634:
631:
629:
626:
624:
621:
619:
616:
614:
611:
609:
606:
604:
601:
599:
596:
594:
593:Muddus plains
591:
589:
586:
584:
583:Borsu surface
581:
580:
578:
576:
575:Paleosurfaces
572:
568:
561:
556:
554:
549:
547:
542:
541:
538:
527:
523:
519:
515:
511:
507:
503:
499:
492:
489:
477:
473:
469:
465:
461:
457:
453:
449:
445:
438:
436:
432:
420:
416:
412:
408:
404:
400:
399:
394:
387:
385:
381:
368:
364:
357:
354:
349:
342:
340:
336:
331:
326:
325:
316:
314:
310:
303:
295:
291:
285:
282:
278:
274:
268:
265:
258:
256:
254:
250:
246:
241:
239:
235:
231:
227:
223:
219:
215:
213:
209:
205:
201:
197:
192:
190:
186:
183:
179:
175:
171:
167:
163:
159:
155:
151:
147:
143:
139:
135:
132:
124:
120:
111:
108:Selection of
106:
97:
81:
65:
49:
35:
19:
1077:
987:Alnö Complex
933:Omberg horst
923:Muhos Graben
872:Söderfjärden
781:Pärvie Fault
771:Lainio Fault
673:Salpausselkä
501:
497:
491:
481:22 September
479:. Retrieved
451:
447:
424:22 September
422:. Retrieved
402:
396:
373:22 September
371:. Retrieved
366:
356:
347:
323:
284:
272:
267:
242:
216:
193:
182:I and A type
118:
116:
1109:Barents Sea
997:Fen Complex
938:Oslo Graben
862:Siljan Ring
753:shear zones
751:Faults and
688:Trollgarden
279:and oceans.
253:Hans Reusch
234:Lake Ladoga
162:Timan Ridge
150:Polar Urals
140:during the
131:pre-Uralian
96:Timan Ridge
1098:Categories
1012:Norra Kärr
867:Sääksjärvi
837:Lappajärvi
743:Structures
623:Strandflat
304:References
238:Ordovician
185:granitoids
174:ophiolites
980:provinces
877:Suvasvesi
526:128410472
476:128973374
222:sediments
166:type area
650:Moraines
294:Schatsky
277:terranes
158:Varanger
110:outcrops
978:igneous
976:Lesser
847:Lumparn
506:Bibcode
456:Bibcode
407:Bibcode
218:Erosion
212:Arctida
164:is the
138:Baltica
123:Russian
882:Tvären
817:Dellen
524:
474:
152:, the
134:orogen
522:S2CID
472:S2CID
232:near
204:plate
154:Kanin
146:Urals
852:Mien
502:423A
483:2015
426:2015
375:2015
259:Note
247:and
187:and
156:and
117:The
514:doi
464:doi
452:440
415:doi
332:–3.
273:not
1100::
520:.
512:.
500:.
470:.
462:.
450:.
446:.
434:^
413:.
403:12
401:.
395:.
383:^
338:^
312:^
240:.
180:.
125::
559:e
552:t
545:v
528:.
516::
508::
485:.
466::
458::
428:.
417::
409::
377:.
330:1
121:(
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
