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PALYGORSKITE MINERALIZATION IN THE ATOTONILCO EL GRANDE FORMATION (HIDALGO, MEXICO): IMPLICATIONS FOR CATALYTIC APPLICATIONS

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NOVEMBER 2025   -  Volume: 100 -  Pages: 532-537

DOI:

https://doi.org/10.52152/D11467

Authors:

VANESA SANDOVAL - JUAN HERNANDEZ AVILA - EDUARDO CERECEDO SAENZ - ABRAHAM HERNANDEZ GONZALEZ - JAVIER FLORES BADILLO - MANUEL SALDAÑA PINO - ELEAZAR SALINAS RODRIGUEZ - ESTEFANIA ESPINOSA MORALES - JULIO CESAR JUAREZ TAPIA - SURIZHADAY ALCANTARA HERNANDEZ

Disciplines:

  • ATMOSPHERIC SCIENCES (OTRAS ESPECIALIDADES )

Downloads:   11

How to cite this paper:  
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Received Date :   3 June 2025

Reviewing Date :   9 June 2025

Accepted Date :   18 September 2025


Key words:
Mineralization, Palygorskite, Atotonilco el Grande Formation, Catalysis, Rift, Lithium, Dolomite, Siderite, Mineralogical Characterization, Industrial Minerals, X-ray Photoelectron Spectroscopy (XPS), Scanning Electron Microscopy (SEM-EDS), Lithium-bearing clay, Geochemistry, Mexico.
Article type:
ARTICULO DE INVESTIGACION / RESEARCH ARTICLE
Section:
RESEARCH ARTICLES

From an industrial perspective, palygorskite exhibits promising potential as a catalytic support, adsorbent, and cementitious additive. Dolomite complies with national and international standards for use in cement, metallurgy, and agriculture. Siderite constitutes a viable ferrous iron source, although its suitability in ordinary Portland cement requires further evaluation.
Palygorskite, dolomite, and siderite from the Atotonilco el Grande Formation (Hidalgo, Mexico), located in a Pliocene rift-type geodynamic setting, were mineralogically characterized. Indirect exploration methods and advanced analytical techniques were employed, including X-ray diffraction (XRD), X-ray photoelectron spectroscopy (XPS), scanning electron microscopy with energy-dispersive spectroscopy (SEM–EDS), Fourier-transform infrared spectroscopy (FTIR), and gravity separation using a Wilfley shaking table.
The results confirmed the presence of fibrous monoclinic palygorskite (PDF 96-901-0433), dominant dolomite (PDF 96-900-3518), and minor siderite (PDF 96-901-5686). XPS analysis revealed lithium (~0.3?%) in the palygorskite matrix, representing a novel finding for rift-related environments in Mexico. Gravity separation enabled effective isolation of each mineral phase based on density, facilitating detailed individual characterization.
This work represents a pioneering contribution to the study of lithium-bearing clays and industrial carbonates in Mexican rift environments, with potential applications in strategic sectors such as catalysis, energy, metallurgy, environmental remediation, and construction.
Key Words: Mineralization; Palygorskite; Atotonilco el Grande Formation; Catalysis; Rift.

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