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Preliminary U/Th dating and the evolution of gypsum crystals in Naica caves (Mexico)

Sanna, Laura and Forti, Paolo and Lauritzen, Stein-Erik (2011) Preliminary U/Th dating and the evolution of gypsum crystals in Naica caves (Mexico). Acta Carsologica, Vol. 40 (1), p. 17-28. ISSN 0583-6050. Article.

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The origin and the evolution of giant selenite crystals in Naica caves, together with the understanding of their growth mechanisms, is one of the aims of the international multidisciplinary research, called the “Naica Project”. In this context, the exact timing of when the gypsum nucleation started and whether its growth has been constant over time, have been investigated. The preliminary data obtained with the U–Th disequilibrium method show significant differences in ages for gypsum (between 191 ± 13 kyr for one of the Ojo de la Reina cave crystals and 57 ± 1.7 kyr for the base of Espadas cave’s spar) and produced a coarse chronological interval of growth. The crystal depositional rates vary from 0.56 to 1.22 mm/kyr, in excellent agreement with the laboratory tests for gypsum deposition under present conditions performed in the deepest part of the mine. These results are also consistent with a multistage precipitation started at different times in the Naica caves (first in caves at the upper level, where gypsum was subsequently dissolved, and only later in the deeper part of the aquifer under stable conditions) and allow us to improve the knowledge on the speleogenetic evolution of these caves.

Item Type:Article
ID Code:6658
Uncontrolled Keywords:U-Th dating, gypsum speleothems, mine caves, crystal growth rate, Naica, Mexico
Subjects:Area 04 - Scienze della terra > GEO/09 Georisorse minerarie e applicazioni mineralogico- petrografiche per l'ambiente ed i beni culturali
Divisions:001 Università di Sassari > 01 Dipartimenti > Scienze botaniche, ecologiche e geologiche
Publisher:Slovenian Academy of Sciences and Arts, Scientific Research Center of the Slovenian Academy of Sciences and Arts
Deposited On:23 Nov 2011 13:36

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