Erionite series minerals in felsic volcanic rocks of southern Mesa Central, Guanajuato, Mexico

Trace quantities of erionite series minerals were identified along with chabazite, clinoptilolite, and morderite within Chichindaro rhyolites (~ 30 Ma) at latitude 21°8′30″–21°17′00″ and longitude 101°5′00″–101°10′00″, ~ 15 km south of the present-day town of San Felipe in the state of Guanajuato, M...

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Veröffentlicht in:Environmental earth sciences 2021-10, Vol.80 (19), Article 674
Hauptverfasser: Kshirsagar, Pooja, Miranda-Avilés, Raúl, Loza-Aguirre, Isidro, Li, Yanmei, Alquiza, María Jesús Puy y, Moncada-Sánchez, Cristina Daniela, Romo, Karen Arlete Navarro, Hernández-Jiménez, Athziri
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Sprache:eng
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Zusammenfassung:Trace quantities of erionite series minerals were identified along with chabazite, clinoptilolite, and morderite within Chichindaro rhyolites (~ 30 Ma) at latitude 21°8′30″–21°17′00″ and longitude 101°5′00″–101°10′00″, ~ 15 km south of the present-day town of San Felipe in the state of Guanajuato, Mexico. Special attention was given to the erionite -K, Na, and Ca varieties. Despite their occurrence in trace amounts, image analyses of these minerals with the aid of Scanning Electron Microscope indicates the existence of both hair-like and needle-like fibers that are 5.85–29.26 μm long and 2.510–0.252 μm thick, which allows them to be categorized as “inhalable” (with length > 5 μm and thickness 
ISSN:1866-6280
1866-6299
DOI:10.1007/s12665-021-09972-1