"Isaacson, P. E." . . "Late Devonian (Famennian) Glaciation in south America and marine offlap on other continents." . . . "Jian-Wei, S." . "RIV/67985831:_____/99:09004018!RIV/2003/AV0/A09003/N" . "Abhandlungen der Geologischen Bundesanstalt" . "0016-7800" . "239;257" . . "0"^^ . . "0"^^ . "[6DB85A15F3A8]" . "744572" . "1"^^ . "Late Devonian (Famennian) Glaciation in south America and marine offlap on other continents."@en . "P(GA205/96/0137), P(GA205/98/1347), P(IAA3013809), Z(AV0Z3013912)" . . "N/A"@en . "Kalvoda, J." . . "19"^^ . . . . "Hladil, Jind\u0159ich" . . "Given the present data on duration of Devonian stages, Famennian events present a more significant timespan than earlier acknowledged, although thickness of relevant sediments is remarkably reduced. In southern China, aggradation, siliclastic influx, dolomitization from evaporation, and shallow-water carbonates resulted from Famennian se-level lowering. The coupling of glacial and lowstand events explains the sudden appearance of shallow-marine, as well as subaerially-affected features within a generally transgressive sea that breached the North American craton during Late Devonian (Frasnian) time."@en . "5"^^ . "AT - Rakousk\u00E1 republika" . "Given the present data on duration of Devonian stages, Famennian events present a more significant timespan than earlier acknowledged, although thickness of relevant sediments is remarkably reduced. In southern China, aggradation, siliclastic influx, dolomitization from evaporation, and shallow-water carbonates resulted from Famennian se-level lowering. The coupling of glacial and lowstand events explains the sudden appearance of shallow-marine, as well as subaerially-affected features within a generally transgressive sea that breached the North American craton during Late Devonian (Frasnian) time." . . . . . "RIV/67985831:_____/99:09004018" . "Late Devonian (Famennian) Glaciation in south America and marine offlap on other continents."@en . "54" . . . "Grader, G." . "N/A" . "Late Devonian (Famennian) Glaciation in south America and marine offlap on other continents." .