The caves located within the Pb-Zn mine of Naica (Chiuhahua, Mexico) constitute a unique karstic environment because they lack a direct interconnection with the surface environment, and because they host exceptionally big selenite crystals (>10m in length). We report on an ongoing multidisciplinary study that considers the entire extent of the cave system and that is based on a large set of fluid inclusion, isotopic, and palynological data. This data set is used to propose a genetic model of the giant crystals.

A tale of precipitation and groth of giant selenite crystals within the caves of Naica (Chihahua, Mexico) / P. S., Garofalo; M., Fricker; D., Gunther; P., Forti; S. E., Lauritzen; Mercuri, Anna Maria; M., Loreti. - STAMPA. - (2008), pp. 158-159. (Intervento presentato al convegno III All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium tenutosi a Moscow nel 22-25/09/2008).

A tale of precipitation and groth of giant selenite crystals within the caves of Naica (Chihahua, Mexico)

MERCURI, Anna Maria;
2008

Abstract

The caves located within the Pb-Zn mine of Naica (Chiuhahua, Mexico) constitute a unique karstic environment because they lack a direct interconnection with the surface environment, and because they host exceptionally big selenite crystals (>10m in length). We report on an ongoing multidisciplinary study that considers the entire extent of the cave system and that is based on a large set of fluid inclusion, isotopic, and palynological data. This data set is used to propose a genetic model of the giant crystals.
2008
III All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium
Moscow
22-25/09/2008
158
159
P. S., Garofalo; M., Fricker; D., Gunther; P., Forti; S. E., Lauritzen; Mercuri, Anna Maria; M., Loreti
A tale of precipitation and groth of giant selenite crystals within the caves of Naica (Chihahua, Mexico) / P. S., Garofalo; M., Fricker; D., Gunther; P., Forti; S. E., Lauritzen; Mercuri, Anna Maria; M., Loreti. - STAMPA. - (2008), pp. 158-159. (Intervento presentato al convegno III All-Russian conference on thermobarogeochemistry in conjunction with IV APIFIS symposium tenutosi a Moscow nel 22-25/09/2008).
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11380/754454
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