Zobrazeno 1 - 7
of 7
pro vyhledávání: '"neoproterozoikum"'
Autor:
Zieger-Hofmann, Mandy
There exist various glacial units in the Neoproterozoic strata of southern Namibia (Kalahari Craton). They were recognised and discussed in the scientific literature for at nearly 100 years (e.g. Coleman, 1926; Gevers, 1931; Schwellnuss, 1941; Martin
Externí odkaz:
https://tud.qucosa.de/id/qucosa%3A84016
https://tud.qucosa.de/api/qucosa%3A84016/attachment/ATT-0/
https://tud.qucosa.de/api/qucosa%3A84016/attachment/ATT-0/
Autor:
Santolík, Václav
The Davle Volcanic Complex (DVC) situated in the Teplá-Barrandian unit (TBU) of the Bohemian Massif, is considered as a Neoproterozoic-Cambrian magmatic arc that developed on the northern active margin of Gondwana supercontinent during Cadomian accr
Externí odkaz:
http://www.nusl.cz/ntk/nusl-447468
Autor:
Santolík, Václav
The Davle Volcanic Complex (DVC) situated in the Teplá-Barrandian unit (TBU) of the Bohemian Massif, is considered as a Neoproterozoic-Cambrian magmatic arc that developed on the northern active margin of Gondwana supercontinent during Cadomian accr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::039d09768a12342998df4976a9c0b743
http://www.nusl.cz/ntk/nusl-447468
http://www.nusl.cz/ntk/nusl-447468
Autor:
Mráček, Michal
Diploma thesis deals with geological, petrological, structural and geochemical studies of the most probably neoproterozoic volcanic and sedimentary rocks of the Pičín belt in the area NW from Dobříš, approximately between the villages Trnová an
Externí odkaz:
http://www.nusl.cz/ntk/nusl-334693
Autor:
Mráček, Michal
Diploma thesis deals with geological, petrological, structural and geochemical studies of the most probably neoproterozoic volcanic and sedimentary rocks of the Pičín belt in the area NW from Dobříš, approximately between the villages Trnová an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::56c15780b2a73dd28e3db1ef83a3ed1a
http://www.nusl.cz/ntk/nusl-334693
http://www.nusl.cz/ntk/nusl-334693
Autor:
Helbing, Heiko
Der SE-Rand des Luswishi Dome gehört zum Zentrum des metamorphen Kernbereichs (Domes Region) des pan-afrikanischen Lufilian Belt in Sambia. Stratigraphische, strukturelle, texturelle und petrologische Daten belegen eine polyphase Überprägung am SE
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______707::5cef88b3fa33554d170f80fe97435f3e
https://hdl.handle.net/10900/48583
https://hdl.handle.net/10900/48583