Sedimentology and stratigraphy of the vaca muerta formation in the cerro Domuyo area, northern Neuquén, Argentina
The Vaca Muerta Formation in the Cerro Domuyo area shows an interesting intercalation of facies with opposite paleocurrents. The unit is represented by outer ramp to basinal facies with a westward direction of progradation. However, in its middle section, slope deposits correlatable with the Huncal...
Guardado en:
| Publicado: |
2013
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v40_n1_p41_Kietzmann http://hdl.handle.net/20.500.12110/paper_07187092_v40_n1_p41_Kietzmann |
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