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Isabel Méndez-Bedia,Gloria Gallastegui,Pedro Busquets,Silvia N. Césari,Carlos O. Limarino,Eva Prats,Raúl Cardó,Ferrán Colombo
Pág. 275 - 294
In the Argentinian Andes (Frontal Cordillera) the upper part of the late Carboniferous-early Permian San Ignacio Formation is made up of lacustrine-palustrine microbial carbonates and interbedded volcanic deposits. In this lacustrine-palustrine environme...
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Rodrigo Braga Moruzzi, Lais Galileu Speranza, Fabiano Tomazini da Conceição, Suely Teodoro de Souza Martins, Rosa Busquets and Luiza Cintra Campos
Stormwater runoff carries pollutants from urban areas to rivers and has the potential to be a main contributing source of microplastics (MPs) to the ecosystem. Stormwater detention reservoirs (SDRs) differ from ponds and lakes in that SDRs retain most pa...
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Pedro Busquets,Carlos Oscar Limarino,Raúl Cardó,Isabel Méndez-Bedia,Gloria Gallastegui,Ferrán Colombo,Nemesio Heredia,Silvia N. Césari
Pág. 172 - 195
This paper addresses the stratigraphic analysis of the Late Paleozoicsequence outcroping in the Sierra de Castaño area (Cordillera Frontal, San Juan Province, Argentina). In this region three major stratigraphic units have been recognized. The lower one ...
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J. J. Candel, V. Amigó, J. A. Ramos, D. Busquets
Pág. 340 - 350
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Mario Pino,Tamara Busquets,Robert Brümmer
Pág. 187 - 204
Microtidal flood plain estuaries are well represented along the coast of south - central Chile (ca. 35 - 41°S). The Queule River estuary (39°23'S, 73°12'W) has a small tidal flat, which formed after the earthquake and tsunami of May 1960 and is made up o...
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Xavier Busquets, Juan Batanero, Ramiro Rodríguez-Borlado, Carlos Martínez Lasheras, Rafael Martínez Lasheras
Pág. 57 - 78
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