31:
582:
568:
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,
206:
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
594:
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).
556:
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,
581:
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,
368:
Thybo, H. (1997). "Geophysical characteristics of the
Tornquist Fan area, northwest Trans-European Suture Zone: Indication of late Carboniferous to early Permian dextral transtension".
583:
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
482:
Narkiewicz, M; et al. (2015). "Transcurrent nature of the
Teisseyre–Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile".
320:, 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
484:
58: ). 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.
664:
639:
256:
596:"Transcurrent nature of the Teisseyre–Tornquist Zone in Central Europe: results of the POLCRUST-01 deep reflection seismic profile"
321:
273:
276:
under the
Tornquist Fan has a strong topography with depths varying between 26 and 48 km. It started forming during the
406:
659:
644:
324:
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
684:
674:
669:
654:
649:
370:
679:
414:
215:
187:
109:. The south-eastern part of the zone, now largely concealed by deep sedimentary basins, developed through
689:
249:
423:
347:
183:
179:
144:
102:
75:
253:
191:
241:
501:
451:"Upper mantle structure around the Trans-European Suture Zone obtained by teleseismic tomography"
387:
277:
344: – Sea between the palaeocontinents Avalonia and Baltica about 600 to 450 million years ago
570:
615:
523:
607:
493:
462:
431:
379:
166:
The latter two branches (STZ and TEF) span a triangular area of numerous faults, called the
110:
65:
30:
106:
17:
245:
427:
539:
332:
sediments, and located further west than indicated by historical surface observations.
211:
114:
435:
633:
505:
391:
341:
546:. Geological Society, London, Special Publications. Vol. 434. pp. 127–147.
34:
Geologic map of Europe showing the Baltic Shield and East
European Platform (
27:
Boundary between the East
European Craton and the orogens of South-Western Europe
219:
79:
186:. As part of his work on a Geological Atlas of Galicia he mapped the line from
611:
535:
497:
383:
309:
619:
540:"Disrupted vegetation as a response to Jurassic volcanism in southern Sweden"
595:
325:
317:
305:
293:
207:
90:
86:
557:
520:
Wawrzyniec Karol de
Teisseyre: A Pioneer in the Study of "Cryptotectonics"
222:. It includes the following linear features (sorted from the north-east):
542:. In Kear, B.P.; Lindgren, J.; Hurum, J.H.; MilĂ n, J.; Vajda, V. (eds.).
467:
450:
329:
285:
231:
140:
94:
313:
289:
281:
236:
The
Sorgenfrei-Tornquist Zone (STZ), including many parallel horsts in
98:
237:
227:
195:
136:
93:. The north-western part of the zone was created by the collision of
82:
29:
190:
in Ukraine to south-eastern Poland. In 1908 the German geologist
182:
suggested the existence of a buried tectonic line close to the
571:
http://onlinelibrary.wiley.com/doi/10.1002/2015TC003934/full
524:
http://onlinelibrary.wiley.com/doi/10.1029/2002EO000370/pdf
292:. Faults are believed to have continued forming until late
544:
Mesozoic Biotas of Scandinavia and its Arctic Territories
252:
in the Jurassic. In association to this event numerous
120:
Various branches of the TESZ go under different names:
38: ) and European orogenic belts (Caledonian
304:The Teisseyre-Tornquist Zone (TTZ), extending from
194:mapped the continuation of the zone from Poland to
74:, is the crustal boundary between the Precambrian
407:"the Tornquist Sea and baltica-Avalonia docking"
85:of South-Western Europe. The zone runs from the
538:; Linderson, Hans; McLoughlin, Stephen (2016).
405:Torsvik, Trond H.; Rehnström, Emma F. (2003).
8:
466:
558:http://2dgf.dk/xpdf/bull46-2-145-160.pdf
600:International Journal of Earth Sciences
522:, Eos, Vol. 83, No. 47, pages 541-556,
485:International Journal of Earth Sciences
360:
226:The Fennoscandian Border Zone (FBZ) in
7:
280:as a microcontinent or a series of
265:Caledonian Deformation Front (CDF)
25:
518:R. Teisseyre and B. Teisseyre,
449:Janutyte; et al. (2015).
1:
436:10.1016/s0040-1951(02)00631-5
178:In 1893 the Polish geologist
128:(TTZ) in Ukraine and Poland.
257:sprang up in Central Scania
706:
268:Trans-European Fault (TEF)
70:(TESZ), also known as the
18:Trans European Suture Zone
665:Ordovician paleogeography
640:Natural history of Europe
612:10.1007/s00531-014-1116-4
498:10.1007/s00531-014-1116-4
384:10.1017/s0016756897007267
350: – Geology of Europe
262:Ringkøbing-Fyn High (RFH)
248:). This zone experienced
162:through southern Denmark.
133:Sorgenfrei-Tornquist Zone
300:Teisseyre-Tornquist Zone
288:origin amalgamated with
126:Teisseyre-Tornquist Zone
214:which runs between the
59:
50: ; Variscan
254:monogenetic volcanoes
156:Thor-Tornquist Suture
33:
468:10.5194/se-6-73-2015
348:East European Craton
184:Carpathian Mountains
180:Wawrzyniec Teisseyre
152:Trans-European Fault
103:East European Craton
76:East European Craton
54: ; Alpine
428:2003Tectp.362...67T
371:Geological Magazine
192:Alexander Tornquist
660:Geology of Ukraine
645:Geology of Denmark
278:Caledonian orogeny
60:
685:Paleozoic Ukraine
675:Paleozoic Denmark
670:Ordovician Sweden
655:Geology of Sweden
650:Geology of Poland
117:orogenic events.
16:(Redirected from
697:
680:Paleozoic Poland
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107:Late Ordovician
64:Trans-European
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606:(3): 775–796.
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492:(3): 775–796.
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441:
422:(1–4): 67–82.
415:Tectonophysics
397:
378:(5): 597–606.
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358:
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353:
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337:
334:
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270:
269:
266:
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212:Iapetus Suture
203:
200:
175:
172:
164:
163:
148:
135:(STZ) through
129:
72:Tornquist Zone
26:
24:
14:
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10:
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3:
2:
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342:Tornquist Sea
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242:Linderödsåsen
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221:
218:and Scottish
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202:Tornquist Fan
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173:
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168:Tornquist Fan
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145:North Jutland
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19:
690:Suture zones
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216:Scandinavian
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155:
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132:
125:
119:
71:
63:
61:
536:Vajda, Vivi
455:Solid Earth
220:Caledonides
198:in Sweden.
160:Thor Suture
80:Phanerozoic
634:Categories
355:References
310:Baltic Sea
147:(Denmark).
139:(Sweden),
620:1437-3262
506:129630403
461:: 73–91.
392:129418419
326:Paleozoic
318:Black Sea
306:Pomerania
294:Paleozoic
286:Avalonian
250:extension
246:Söderåsen
208:North Sea
174:Discovery
91:Black Sea
87:North Sea
336:See also
330:Mesozoic
282:terranes
232:Kattegat
210:and the
141:Kattegat
111:Variscan
95:Avalonia
78:and the
424:Bibcode
316:at the
314:Dobruja
312:to the
308:at the
290:Baltica
188:Galicia
154:(TEF),
105:in the
99:Baltica
89:to the
83:orogens
618:
504:
390:
240:(e.g.
238:Scania
228:Skagen
196:Scania
143:, and
137:Scania
115:Alpine
66:Suture
56:
52:
48:
44:
40:
36:
502:S2CID
410:(PDF)
388:S2CID
616:ISSN
328:and
322:Moho
274:Moho
272:The
244:and
230:and
150:The
131:The
124:The
113:and
97:and
68:Zone
62:The
608:doi
604:104
494:doi
490:104
463:doi
432:doi
420:362
380:doi
376:134
284:of
158:or
636::
614:.
602:.
598:.
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374:.
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170:.
622:.
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508:.
496::
471:.
465::
459:6
438:.
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394:.
382::
259:.
101:/
20:)
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