Zobrazeno 1 - 10
of 193
pro vyhledávání: '"Manuel POZO"'
Autor:
Francisco Franco, Juan Antonio Cecilia, Laura Pardo, Salima Essih, Manuel Pozo, Lucía dos Santos-Gómez, Rosario M. P. Colodrero
Publikováno v:
Nanomaterials, Vol 14, Iss 18, p 1532 (2024)
Addressing climate change requires transitioning to cleaner energy sources and adopting advanced CO2 capture techniques. Clay minerals are effective in CO2 adsorption due to their regenerative properties. Recent advancements in nanotechnology further
Externí odkaz:
https://doaj.org/article/3616f2518ad54a0589ab538570ddaa33
Autor:
Vanina Rodríguez-Ameijide, Andrea Maggio, Manuel Pozo, M. Belén Gómez, Pablo M. Naranjo, M. Eugenia Roca-Jalil
Publikováno v:
Minerals, Vol 14, Iss 2, p 133 (2024)
In the northern Patagonian region of Argentina, some of the largest bentonite deposits exist. Four bentonite samples (B1, B2, B3, and B4) from two deposits were thoroughly characterised and evaluated as potential adsorbents of anthocyanins extracted
Externí odkaz:
https://doaj.org/article/8b456e47bf6a40c781a3952715e07212
Autor:
Micaela A. Sanchez, Miria T. Baschini, Manuel Pozo, Betina R. Gramisci, María E. Roca Jalil, María L. Vela
Publikováno v:
Materials, Vol 16, Iss 14, p 5062 (2023)
The Copahue Thermal Center, situated in Neuquén, Argentina, produces natural and matured peloids, which are employed in the prevention and treatment of various osteoarticular and dermatological disorders. The presence of sulfur as a constituent and
Externí odkaz:
https://doaj.org/article/3b3b3d34d01641548c10e730698aa9a9
Autor:
Juan Emilio Herranz, Manuel Pozo
Publikováno v:
Minerals, Vol 12, Iss 8, p 987 (2022)
Lithofacies belonging to mud-flat and palustrine deposits (lake margin) in the Miocene of the Madrid Basin (Spain) have been studied. Four lithofacies corresponding to mud flat (1 and 3) and palustrine (2 and 4) deposits have been differentiated. Uni
Externí odkaz:
https://doaj.org/article/f87043863fc544c69011a3c026ec337b
Publikováno v:
Minerals, Vol 12, Iss 4, p 467 (2022)
Collected samples of bentonite and associated facies from the Justina deposit of Cretaceous age (Anacleto Formation) have been studied. Facies analysis, mineralogical, and geochemical studies have been carried out using several techniques, including:
Externí odkaz:
https://doaj.org/article/2f4ed7fcd505485ebea3e43ad51bd593
Autor:
Maria Isabel Prudêncio, Francisco Ruiz, Rosa Marques, Maria Isabel Dias, Joaquín Rodríguez Vidal, Ana Luísa Rodrigues, Luis Miguel Cáceres, María Luz González-Regalado, Juan Manuel Muñoz, Manuel Pozo, Paula Gómez, Antonio Toscano, Manuel Abad, Tatiana Izquierdo, Marta Arroyo, Verónica Romero, Gabriel Gómez
Publikováno v:
Minerals, Vol 12, Iss 4, p 417 (2022)
The Tinto and Odiel rivers (SW Spain) drain from a vast sulfide mining district and join at a 20-km-long estuary that enters the Atlantic Ocean. In this work, the contents of rare earth elements (REE) and fractionation in Neogene–Holocene sediment
Externí odkaz:
https://doaj.org/article/3730ac5664f446ff9fc03036a91fc915
Autor:
Liliana Guerra, Cristina Veiga-Pires, María Luz González-Regalado, Manuel Abad, Antonio Toscano, Juan Manuel Muñoz, Francisco Ruiz, Joaquín Rodríguez Vidal, Luis Miguel Cáceres, Tatiana Izquierdo, María Isabel Carretero, Manuel Pozo, Guadalupe Monge, Josep Tosquella, Paula Gómez, Verónica Romero, Marta Arroyo, Gabrlel Gómez
Publikováno v:
Estudios Geologicos, Vol 76, Iss 2, Pp e131-e131 (2020)
Durante el periodo romano (siglo III a.C.-siglo V d.C.), las zonas próximas a la actual desembocadura del río Guadalquivir estaban ocupadas por una laguna interior con conexión marina, a partir de la interpretación paleoambiental de las asociacio
Externí odkaz:
https://doaj.org/article/f8900251c63848beb76f6d0b7b506f9e
Autor:
Paulo R. A. Netto, Manuel Pozo, Maurício Dias da Silva, Márcia Elisa Boscato Gomes, André Mexias, Camila Wense Ramnani, Yaro Parizek-Silva, Leonardo Borghi, Aristóteles de Moraes Rios-Netto
Publikováno v:
Minerals, Vol 12, Iss 2, p 200 (2022)
The characterization of Mg-clays in rock samples (well P1) from the Barra Velha Formation (Early Cretaceous) allowed the establishment of mineral assemblages on the basis of their kerolite and Mg-smectite (stevensite and saponite) content. Kerolite-r
Externí odkaz:
https://doaj.org/article/5b4d4e0127b34699bc0f52abfcf0e2e9
Autor:
Francisco Ruiz, Manuel Pozo, María Luz González-Regalado, Joaquín Rodríguez Vidal, Luis Miguel Cáceres, Manuel Abad, Tatiana Izquierdo, María Isabel Prudencio, María Isabel Dias, Rosa Marques, Juan M. Muñoz-Pichardo, Josep Tosquella, Paula Gómez, Antonio Toscano, Verónica Romero, Marta Arroyo
Publikováno v:
Minerals, Vol 11, Iss 12, p 1397 (2021)
This paper presents the easternmost mineralogical and geochemical evidence of the 1755 Lisbon tsunami found in the Western Mediterranean. This multidisciplinary analysis of a sediment core obtained in Gibraltar (southern Iberian Peninsula) has allowe
Externí odkaz:
https://doaj.org/article/bc360152daf24311becc77a029f46a3a
Autor:
Maurício Dias da Silva, Márcia Elisa Boscato Gomes, André Sampaio Mexias, Manuel Pozo, Susan Martins Drago, Raquel Severo Célia, Luis Adriano Carvalho Silva, Paulo Netto, Lucas Bonan Gomes, Carla Cristine Porcher, Norberto Dani, Deborah Driemeyer, Camila Wense Dias Ramnani, Julice Ferreira Santos
Publikováno v:
Minerals, Vol 11, Iss 9, p 970 (2021)
The object of this study is magnesian clay minerals present in carbonate rocks of the post-rift phase of the pre-salt in the Santos Basin. These rocks developed in an Aptian-age alkaline lacustrine environment. This study summarizes the formation of
Externí odkaz:
https://doaj.org/article/53de9e8ec49e4385b14678964c9c2179