Zobrazeno 1 - 10
of 213
pro vyhledávání: '"kerolite"'
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
Publikováno v:
Minerals, Vol 12, Iss 5, p 650 (2022)
Nickel weathering ores are used to produce metallic nickel, stainless steels, and nickel sulfate, the main component of batteries. The global production of nickel from weathering ores is increasing and has surpassed production from sulfide magmatic d
Externí odkaz:
https://doaj.org/article/51fa6fb8ced645ad99ea6fac14f7e405
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
Akademický článek
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Autor:
Sufriadin Sufriadin, Arifudin Idrus, S. Pramumijoyo, I. W. Warmada, I. Nur, A. Imai, A. M. Imran, Kaharuddin Kaharuddin
Publikováno v:
Indonesian Journal on Geoscience, Vol 7, Iss 2, Pp 77-85 (2014)
DOI: 10.17014/ijog.v7i2.137Mineralogical characterization of some garnierite samples from Soroako have been conducted using X-ray diffraction, thermal analysis, and infrared spectroscopy methods. XRD patterns reveal the samples mainly containing the
Externí odkaz:
https://doaj.org/article/9eb853a846c34948b05c0b931424089f
Publikováno v:
Minerals, Vol 9, Iss 11, p 696 (2019)
A review and a synthesis of the geological, mineralogical, and crystal chemical data available in the literature on active Spanish bentonitic exploitations were done, and at the same time, new data are provided from a set of representative samples fr
Externí odkaz:
https://doaj.org/article/940a3c6c7b5045bc9a75334df29c571b
Autor:
Raquel Severo Célia, Carla Cristine Porcher, Paulo Netto, Norberto Dani, Mauricio Dias da Silva, Andre Sampaio Mexias, Susan Martins Drago, Julice Ferreira Santos, Lucas Bonan Gomes, Manuel Pozo, Camila Wense Dias Ramnani, Marcia Elisa Boscato Gomes, Deborah Driemeyer, Luis Adriano Carvalho Silva
Publikováno v:
Minerals, Vol 11, Iss 970, p 970 (2021)
Minerals
Volume 11
Issue 9
Minerals
Volume 11
Issue 9
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
Publikováno v:
Geochimica et Cosmochimica Acta. 288:301-315
The magnesium silicate mineral sepiolite is an important component of both alkaline lake and siliceous marine sediments. However, apart from historical constraints on its equilibrium solubility and effective solubility in surface waters, little is kn
Autor:
Jennifer L. Bentz, Ronald C. Peterson
Publikováno v:
Clays and Clay Minerals. 68:115-134
Understanding clay-mineral assemblages forming in saline lakes aids in reconstructing paleoenvironments on Earth and other terrestrial planets; this is because authigenic phyllosilicates are sensitive to the prevailing geochemical conditions present
Publikováno v:
Clays and Clay Minerals. 67:488-506
When present at elevated levels in drinking water, arsenic is toxic, and magnesian clays are gaining recognition as a source of elevated arsenic in groundwater. In the crust and upper mantle of Earth, arsenic incorporation into clay minerals is influ