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Von der Anchizone bis zur Eklogitfazies: Angekippte Krustenprofile als Folge der cadomischen und variscischen Orogenese im Teplá-Barrandium (Böhmische Masse)
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Zulauf G. Von der Anchizone bis zur Eklogitfazies: Angekippte Krustenprofile als Folge der cadomischen und variscischen Orogenese im Teplá-Barrandium (Böhmische Masse). Geotekt. Forsch. 1997, 89:1-302.
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(1997)
Geotekt. Forsch.
, vol.89
, pp. 1-302
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Zulauf, G.1
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