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Economic Geology; June-July; v. 103; no. 4; p. 865-869; DOI: 10.2113/gsecongeo.103.4.865
© 2008 Society of Economic Geologists
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Scientific Communications

IDENTIFICATION OF AMMONIUM-BEARING MINERALS BY SHORTWAVE INFRARED REFLECTANCE SPECTROSCOPY AT THE ESQUEL GOLD DEPOSIT, ARGENTINA

Walter Soechting1, Nora Rubinstein2,{dagger} and Marta Godeas3

1 Minas Argentinas, San Luis 238, (oeste) San Juan, Argentina
2 Universidad de Buenos Aires-Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), and Departamento de Geología, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Ciudad Universitaria, (1428) Ciudad Autónoma de Buenos Aires, Argentina
3 Servicio Geológico Minero Argentino (SEGEMAR), Av. Julio A. Roca 651, 8° piso, sector 9, (1322) Ciudad Autónoma de Buenos Aires, Argentina

{dagger} Corresponding author: e-mail, nora{at}gl.fcen.uba.ar

The Esquel low-sulfidation epithermal vein deposit in Chubut province, Argentina, is hosted by a Late Jurassic bimodal arc assemblage. Shortwave infrared (SWIR) reflectance spectroscopy of vein samples using a hand-held field spectrometer identified ammonium-bearing illite, jarosite, and adularia (buddingtonite) in banded quartz displaying colloform and crustiform textures. The SWIR technique proved to be a rapid and accurate means of detecting ammonium-bearing species, particularly buddingtonite, which provides evidence for paleoboiling zones and thus of precious metal mineralization.







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