The peloidal tempestites of the Vaca Muerta Formation (Tithonian- Valanginian) in the southern Mendoza sector of the Neuquén Basin, Argentina
Storm deposits (tempestites) have been extensively studied in the sedimentary record, particularly those deposits with hummocky cross-stratification, knowing their bathymetric ranks, facies models and their hydrodynamic conditions (Harms et al., 1975; Dott y Burgeois, 1982; Dumas y Arnott, 2006). Ho...
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| Autores principales: | Kietzmann, D.A., Palma, R.M. |
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| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_16697316_v18_n2_p121_Kietzmann |
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