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Dallmeyer, R. D., Urban, M. (1998) Variscan vs Cadomian tectonothermal activity in northwestern sectors of the Teplá-Barrandian zone, Czech Republic: constraints from 40 Ar/ 39 Ar ages. Geologische Rundschau, 87 (1) 94-106 doi:10.1007/s005310050192

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Reference TypeJournal (article/letter/editorial)
TitleVariscan vs Cadomian tectonothermal activity in northwestern sectors of the Teplá-Barrandian zone, Czech Republic: constraints from 40 Ar/ 39 Ar ages
JournalGeologische Rundschau
AuthorsDallmeyer, R. D.Author
Urban, M.Author
Year1998 (May 20)Volume87
Issue1
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s005310050192Search in ResearchGate
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Mindat Ref. ID512504Long-form Identifiermindat:1:5:512504:7
GUID0
Full ReferenceDallmeyer, R. D., Urban, M. (1998) Variscan vs Cadomian tectonothermal activity in northwestern sectors of the Teplá-Barrandian zone, Czech Republic: constraints from 40 Ar/ 39 Ar ages. Geologische Rundschau, 87 (1) 94-106 doi:10.1007/s005310050192
Plain TextDallmeyer, R. D., Urban, M. (1998) Variscan vs Cadomian tectonothermal activity in northwestern sectors of the Teplá-Barrandian zone, Czech Republic: constraints from 40 Ar/ 39 Ar ages. Geologische Rundschau, 87 (1) 94-106 doi:10.1007/s005310050192
In(1998, May) Geologische Rundschau Vol. 87 (1) Springer Science and Business Media LLC

See Also

These are possibly similar items as determined by title/reference text matching only.

Dallmeyer, R. D., Urban, M. (1994) Variscan vs. Cadomian tectonothermal evolution within the Teplá-Barrandian Zone, Bohemian Massif, Czech Republic: evidence from 40Ar/39Ar mineral and whole-rock slate/phyllite ages. Journal of the Czech Geological Society, 39 (1) 21
Handler, R., Dallmeyer, R. D., Neubauer, F. (1997) 40 Ar/ 39 Ar ages of detrital white mica from Upper Austroalpine units in the Eastern Alps, Austria: Evidence for Cadomian and contrasting Variscan sources. Geologische Rundschau, 86 (1) 69-80 doi:10.1007/s005310050122
Goodge, John W., Dallmeyer, R. D. (1992) $$^{40}Ar/^{39}Ar$$ Mineral Age Constraints on the Paleozoic Tectonothermal Evolution of High-Grade Basement Rocks within the Ross Orogen, Central Transantarctic Mountains. The Journal of Geology, 100 (1) 91-106 doi:10.1086/629573
Dallmeyer, R. D., Neubauer, F., Fritz, H., Putiš, M. (1994) Variscan vs. Alpine tectonothermal evolution within the Eastern Alps and Western Carpathians, Austria - Slovakia. Journal of the Czech Geological Society, 39 (1) 20
Dallmeyer, R. D., D'Lemos, R. S., Strachan, R. A. (2007) Timing of Cadomian and Variscan tectonothermal activity, La Hague and Alderney, North Armorican Massif: Evidence from 40Ar/39Ar mineral ages. Geological Journal, 29 (1) 29-44 doi:10.1002/gj.3350290104
Dallmeyer, R. D., Gee, D. G., Beckholmen, M. (1985) 40 Ar/ 39 Ar mineral age record of early Caledonian tectonothermal activity in the Baltoscandian Miogeocline, central Scandinavia. American Journal of Science, 285 (6) 532-568 doi:10.2475/ajs.285.6.532
Dallmeyer, R. D., Neubauer, F., Fritz, H., Mocanu, V. (1994) Pre-Variscan, Variscan and Alpine tectonothermal evolution within the southern Carpathians, Romania: evidence from 40Ar/39Ar hornblende and muscovite ages. Journal of the Czech Geological Society, 39 (1) 18-19
Dallmeyer, R.D, Neubauer, F, Fritz, H, Mocanu, V (1998) Variscan vs. Alpine tectonothermal evolution of the Southern Carpathian orogen: constraints from 40Ar/39Ar ages. Tectonophysics, 290 (1) 111-135 doi:10.1016/s0040-1951(98)00006-7
Dörr, Wolfgang, Fiala, Ji q i, Vejnar, Z., Zulauf, Gernold (1998) U–Pb zircon ages and structural development of metagranitoids of the Teplá crystalline complex: evidence for pervasive Cambrian plutonism within the Bohemian massif (Czech Republic) Geologische Rundschau, 87 (1) 135-149 doi:10.1007/s005310050195
Dallmeyer, R. D. (1978) 40 Ar/ 39 Ar incremental-release ages of hornblende and biotite across the Georgia Inner Piedmont; their bearing on late Paleozoic-early Mesozoic tectonothermal history. American Journal of Science, 278 (2) 124-149 doi:10.2475/ajs.278.2.124
Dallmeyer, R. D. (1977) Diachronous ophiolite obduction in western Newfoundland; evidence from 40 Ar/ 39 Ar ages of the Hare Bay metamorphic aureole. American Journal of Science, 277 (1) 61-72 doi:10.2475/ajs.277.1.61
 
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