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, R.A., Concheyro, A., Aberhan, M., Hecht, L., Medina, F.A., Tagle, R.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_01956671_v26_n2_p283_Scasso
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