A tsunami deposit at the Cretaceous/Paleogene boundary in the Neuquén Basin of Argentina

A coarse-grained sandstone bed of Cretaceous/Paleogene (K/Pg) boundary age occurs in a homogeneous neritic shelf mudstone sequence (Jagüel Formation) in the Neuquén Basin of Argentina. This bed, 15 - 25 cm thick, contains abundant plagioclase, broken shells and sharks' teeth. Sedimentological f...

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Autores principales: Scasso, Roberto Adrian, Concheyro, Graciela Andrea, Medina, Francisco Alberto
Publicado: 2005
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v26_n2_p283_Scasso
http://hdl.handle.net/20.500.12110/paper_01956671_v26_n2_p283_Scasso
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