The Carboniferous-Permian Dwyka Group in southern Namibia is subdivided into four upward-fining deglaciation sequences, each of which is capped by finegrained glaciolacustrine or glaciomarine deposits. Both the second and the third deglaciation sequence
U-Pb zircon data from the uppermost Cottons Breccia, representing the Marinoan glacial-postglacial t...
Glacial deposits of Sturtian and Marinoan age occur in the well-studied Neoproterozoic successions o...
International audienceThe response of sediment routing to climatic changes across icehouse-to-greenh...
The Carboniferous-Permian Dwyka Group in southern Namibia is subdivided into four upward-fining degl...
At Zwartbas, about 10 km west of Vioolsdrif, southern Namibia, the Dwyka succession is composed of t...
Glacial deposits of the Dwyka Group between Keetmanshoop and Mariental in southern Namibia have been...
The termination of the Marinoan Snowball Earth glacial epoch was one of the most extreme climate eve...
Bibliography: leaves 238-251.Worldwide most Neoproterozoic sequences are characterised by an intimat...
The Namibian Mesozoic successions may be remnant of a high dynamic sedimentary system that is charac...
The northern Namibian Karoo‐aged successions are part of a Gondwana‐wide sedimentary system emerging...
The Late Carboniferous-Early Permian Itarare Group is a thick glacial unit of the Parana Basin. Five...
Integrated sequence stratigraphic and chemostratigraphic data yield a framework for correlations of ...
The Neoproterozoic Cryogenian (‘Marinoan’) Ghaub Formation of northwestern Namibia represents an imp...
[1] A large (11–15%) negative shift in d13C is observed in shallow water carbonates directly beneath...
International audienceThe Late Paleozoic Ice Age (LPIA) is the longest-lived and most extreme glacia...
U-Pb zircon data from the uppermost Cottons Breccia, representing the Marinoan glacial-postglacial t...
Glacial deposits of Sturtian and Marinoan age occur in the well-studied Neoproterozoic successions o...
International audienceThe response of sediment routing to climatic changes across icehouse-to-greenh...
The Carboniferous-Permian Dwyka Group in southern Namibia is subdivided into four upward-fining degl...
At Zwartbas, about 10 km west of Vioolsdrif, southern Namibia, the Dwyka succession is composed of t...
Glacial deposits of the Dwyka Group between Keetmanshoop and Mariental in southern Namibia have been...
The termination of the Marinoan Snowball Earth glacial epoch was one of the most extreme climate eve...
Bibliography: leaves 238-251.Worldwide most Neoproterozoic sequences are characterised by an intimat...
The Namibian Mesozoic successions may be remnant of a high dynamic sedimentary system that is charac...
The northern Namibian Karoo‐aged successions are part of a Gondwana‐wide sedimentary system emerging...
The Late Carboniferous-Early Permian Itarare Group is a thick glacial unit of the Parana Basin. Five...
Integrated sequence stratigraphic and chemostratigraphic data yield a framework for correlations of ...
The Neoproterozoic Cryogenian (‘Marinoan’) Ghaub Formation of northwestern Namibia represents an imp...
[1] A large (11–15%) negative shift in d13C is observed in shallow water carbonates directly beneath...
International audienceThe Late Paleozoic Ice Age (LPIA) is the longest-lived and most extreme glacia...
U-Pb zircon data from the uppermost Cottons Breccia, representing the Marinoan glacial-postglacial t...
Glacial deposits of Sturtian and Marinoan age occur in the well-studied Neoproterozoic successions o...
International audienceThe response of sediment routing to climatic changes across icehouse-to-greenh...