20:
571:
557:
Mazur, S., M. Mikolajczak, P. Krzywiec, M. Malinowski, V. Buffenmyer, and M. Lewandowski (2015), Is the
Teisseyre-Tornquist Zone an ancient plate boundary of Baltica?, Tectonics, 34, doi:10.1002/2015TC003934,
195:
Whereas the south-eastern part of the TESZ (Teisseyre-Tornquist Zone) is relatively well-confined, the north-western part divides into numerous sutures and faults, which fan out towards the
583:
Narkiewicz, M.; Maksym, A.; Malinowski, M.; Grad, M.; Guterch, A.; Petecki, Z.; Probulski, J.; Janik, T.; Majdański, M.; Środa, P.; Czuba, W.; Gaczyński, E.; Jankowski, L. (2015-04-01).
545:
Hans Thybo, Crustal structure and tectonic evolution of the
Tornquist Fan region as revealed by geophysical methods, Bulletin of the Geological Society of Denmark, Vol. 46, pp. 145-160,
570:
M. Averill, T. Bond, P. Sroda, R. Keller, K.C. Miller: An integrated lithospheric study targeting the Holy Cross
Mountains of the Eastern European Trans-European Suture Zone in Poland,
357:
Thybo, H. (1997). "Geophysical characteristics of the
Tornquist Fan area, northwest Trans-European Suture Zone: Indication of late Carboniferous to early Permian dextral transtension".
572:
https://www.researchgate.net/publication/253472355_An_integrated_lithospheric_study_targeting_the_Holy_Cross_Mountains_of_the_Eastern_European_Trans-European_Suture_Zone_in_Poland
359:
471:
Narkiewicz, M; et al. (2015). "Transcurrent nature of the
Teisseyre–Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile".
309:, is primarily known from geophysical studies. Seismic data and gravity models suggest a strong contrast in crustal thickness, with 28–35 km down to the
47: ). Parts of the Trans-European Suture Zone (STZ, TEF and TTZ) are shown as bands of black colour between the North Sea and the Black Sea.
585:"Transcurrent nature of the Teisseyre–Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile"
473:
265:
under the
Tornquist Fan has a strong topography with depths varying between 26 and 48 km. It started forming during the
395:
653:
628:
245:
313:
to the west of the suture and 42–47 km to the east of it. The suture is believed to be buried under thick upper
310:
262:
98:. The south-eastern part of the zone, now largely concealed by deep sedimentary basins, developed through
648:
633:
673:
663:
658:
643:
638:
668:
403:
204:
176:
440:"Upper mantle structure around the Trans-European Suture Zone obtained by teleseismic tomography"
333: – Sea between the palaeocontinents Avalonia and Baltica about 600 to 450 million years ago
559:
512:
678:
238:
155:
The latter two branches (STZ and TEF) span a triangular area of numerous faults, called the
412:
336:
172:
168:
133:
91:
64:
8:
242:
180:
416:
528:
490:
376:
321:
sediments, and located further west than indicated by historical surface observations.
266:
230:
424:
604:
494:
380:
535:. Geological Society, London, Special Publications. Vol. 434. pp. 127–147.
596:
482:
451:
420:
368:
99:
54:
23:
Geologic map of Europe showing the Baltic Shield and East
European Platform (
95:
16:
Boundary between the East
European Craton and the orogens of South-Western Europe
234:
200:
175:. As part of his work on a Geological Atlas of Galicia he mapped the line from
103:
600:
486:
372:
622:
608:
529:"Disrupted vegetation as a response to Jurassic volcanism in southern Sweden"
330:
19:
584:
546:
509:
Wawrzyniec Karol de
Teisseyre: A Pioneer in the Study of "Cryptotectonics"
211:. It includes the following linear features (sorted from the north-east):
531:. In Kear, B.P.; Lindgren, J.; Hurum, J.H.; MilĂ n, J.; Vajda, V. (eds.).
456:
439:
208:
68:
524:
298:
225:
The
Sorgenfrei-Tornquist Zone (STZ), including many parallel horsts in
314:
306:
294:
282:
196:
82:. The north-western part of the zone was created by the collision of
79:
75:
318:
274:
220:
129:
83:
302:
278:
270:
179:
in Ukraine to south-eastern Poland. In 1908 the German geologist
87:
226:
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184:
171:
suggested the existence of a buried tectonic line close to the
125:
71:
582:
560:
http://onlinelibrary.wiley.com/doi/10.1002/2015TC003934/full
513:
http://onlinelibrary.wiley.com/doi/10.1029/2002EO000370/pdf
281:. Faults are believed to have continued forming until late
533:
Mesozoic Biotas of Scandinavia and its Arctic Territories
523:
241:
in the Jurassic. In association to this event numerous
109:
Various branches of the TESZ go under different names:
27: ) and European orogenic belts (Caledonian
293:The Teisseyre-Tornquist Zone (TTZ), extending from
183:mapped the continuation of the zone from Poland to
63:, is the crustal boundary between the Precambrian
620:
396:"the Tornquist Sea and baltica-Avalonia docking"
393:
74:of South-Western Europe. The zone runs from the
527:; Linderson, Hans; McLoughlin, Stephen (2016).
394:Torsvik, Trond H.; Rehnström, Emma F. (2003).
517:
288:
470:
455:
547:http://2dgf.dk/xpdf/bull46-2-145-160.pdf
437:
18:
589:International Journal of Earth Sciences
511:, Eos, Vol. 83, No. 47, pages 541-556,
474:International Journal of Earth Sciences
215:The Fennoscandian Border Zone (FBZ) in
621:
356:
269:as a microcontinent or a series of
13:
254:Caledonian Deformation Front (CDF)
14:
690:
190:
576:
507:R. Teisseyre and B. Teisseyre,
564:
551:
539:
501:
464:
438:Janutyte; et al. (2015).
431:
387:
350:
1:
425:10.1016/s0040-1951(02)00631-5
343:
167:In 1893 the Polish geologist
162:
117:(TTZ) in Ukraine and Poland.
7:
324:
246:sprang up in Central Scania
10:
695:
257:Trans-European Fault (TEF)
59:(TESZ), also known as the
654:Ordovician paleogeography
629:Natural history of Europe
601:10.1007/s00531-014-1116-4
487:10.1007/s00531-014-1116-4
373:10.1017/s0016756897007267
339: – Geology of Europe
251:Ringkøbing-Fyn High (RFH)
237:). This zone experienced
151:through southern Denmark.
122:Sorgenfrei-Tornquist Zone
289:Teisseyre-Tornquist Zone
277:origin amalgamated with
115:Teisseyre-Tornquist Zone
203:which runs between the
48:
39: ; Variscan
243:monogenetic volcanoes
145:Thor-Tornquist Suture
22:
457:10.5194/se-6-73-2015
337:East European Craton
173:Carpathian Mountains
169:Wawrzyniec Teisseyre
141:Trans-European Fault
92:East European Craton
65:East European Craton
43: ; Alpine
417:2003Tectp.362...67T
360:Geological Magazine
181:Alexander Tornquist
649:Geology of Ukraine
634:Geology of Denmark
267:Caledonian orogeny
49:
674:Paleozoic Ukraine
664:Paleozoic Denmark
659:Ordovician Sweden
644:Geology of Sweden
639:Geology of Poland
106:orogenic events.
686:
669:Paleozoic Poland
613:
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96:Late Ordovician
53:Trans-European
44:
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36:
32:
28:
24:
17:
12:
11:
5:
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595:(3): 775–796.
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563:
550:
538:
516:
500:
481:(3): 775–796.
463:
430:
411:(1–4): 67–82.
404:Tectonophysics
386:
367:(5): 597–606.
348:
347:
345:
342:
341:
340:
334:
326:
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290:
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259:
258:
255:
252:
249:
223:
201:Iapetus Suture
192:
189:
164:
161:
153:
152:
137:
124:(STZ) through
118:
61:Tornquist Zone
15:
9:
6:
4:
3:
2:
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331:Tornquist Sea
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284:
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231:Linderödsåsen
228:
224:
222:
218:
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210:
207:and Scottish
206:
202:
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191:Tornquist Fan
188:
186:
182:
178:
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158:
157:Tornquist Fan
150:
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134:North Jutland
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35:
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21:
679:Suture zones
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553:
541:
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519:
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478:
472:
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443:
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205:Scandinavian
194:
166:
156:
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148:
144:
140:
121:
114:
108:
60:
52:
50:
525:Vajda, Vivi
444:Solid Earth
209:Caledonides
187:in Sweden.
149:Thor Suture
69:Phanerozoic
623:Categories
344:References
299:Baltic Sea
136:(Denmark).
128:(Sweden),
609:1437-3262
495:129630403
450:: 73–91.
381:129418419
315:Paleozoic
307:Black Sea
295:Pomerania
283:Paleozoic
275:Avalonian
239:extension
235:Söderåsen
197:North Sea
163:Discovery
80:Black Sea
76:North Sea
325:See also
319:Mesozoic
271:terranes
221:Kattegat
199:and the
130:Kattegat
100:Variscan
84:Avalonia
67:and the
413:Bibcode
305:at the
303:Dobruja
301:to the
297:at the
279:Baltica
177:Galicia
143:(TEF),
94:in the
88:Baltica
78:to the
72:orogens
607:
493:
379:
229:(e.g.
227:Scania
217:Skagen
185:Scania
132:, and
126:Scania
104:Alpine
55:Suture
45:
41:
37:
33:
29:
25:
491:S2CID
399:(PDF)
377:S2CID
605:ISSN
317:and
311:Moho
263:Moho
261:The
233:and
219:and
139:The
120:The
113:The
102:and
86:and
57:Zone
51:The
597:doi
593:104
483:doi
479:104
452:doi
421:doi
409:362
369:doi
365:134
273:of
147:or
625::
603:.
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446:.
442:.
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375:.
363:.
285:.
159:.
611:.
599::
497:.
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454::
448:6
427:.
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383:.
371::
248:.
90:/
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