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María Lidia Sánchez

National Scientific and Technical Research Council

18

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Cranial and postcranial remains of a new species of Prochelidella (Testudines: Pleurodira: Chelidae) from ‘La Buitrera’ (Cenomanian of Patagonia, Argentina), with comments on the monophyly of this extinct chelid genus from southern Gondwana

2020 Journal of Systematic Palaeontology
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Stratigraphy and facies analysis of the La Chilca Formation, Central Precordillera: Insights on the postglacial Ordovician-Silurian boundary and Early Silurian deposits from Argentina

2018 Geological Journal
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Neuquén Group (Upper Cretaceous): A case of underfilled-overfilled cycles in an Andean foreland basin, Neuquén basin, Argentina

2017 Journal of South American Earth Sciences
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Dinosaur tracks in the Kokorkom Desert, Candeleros Formation (Cenomanian, Upper Cretaceous), Patagonia Argentina: Implications for deformation structures in dune fields

2017 Cretaceous Research
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Stratigraphy and sedimentology of the terminal fan of Candeleros Formation (Neuquen Group), Lower Cretaceous, Neuquen Basin, provinces of Neuquen and Mendoza, Argentina

2015 Andean Geology
- María Lidia Sánchez
- Estefanía Asurmendi
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Hybrid coastal edges in the Neuquén Basin (Allen Formation, Upper Cretaceous, Argentina)

2015 Andean Geology
- Paula Armas
- María Lidia Sánchez
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Sedimentary palaeoenvironment, petrography, provenance and diagenetic inference of the Anacleto Formation in the Neuquén Basin, Late Cretaceous, Argentina

2014 Journal of South American Earth Sciences
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Modelo de depósito de la Formación Cerro Lisandro: lóbulos de desembocadura y deltas de tipo Gilbert. Cretácico superior, región central de cuenca Neuquina, Argentina

2014 Revista Mexicana De Ciencias Geologicas
- María Lidia Sánchez
- Estefanía Asurmendi
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Río Colorado Subgroup (Neuquén Group): Paleosimicity record in the Andean foreland basin, Neuquén basin, Neuquén y Río Negro provinces

2013
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Areniscas eólicas y mareales del Cretácico Superior de la Cuenca Neuquina (Argentina). Análisis petrográfico y de procedencia

2012
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