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Erratum for Franchini et al., Economic Geology 100 (4) 733-764.
Economic Geology; January 2006; v. 101; no. 1; p. 271-274; DOI: 10.2113/101.1.271
© 2006 Society of Economic Geologists
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Errata

ERRATA

The first 20% of the full text of this article appears below.

Figures 6Go, 7Go, and 8Go, which appeared in the paper, "Na-Fe-Ca Alteration and LREE (Th-Nb) Mineralization in Marble and Granitoids of Sierra de Sumampa, Santiago del Estero, Argentina" (Franchini et al., 2005, v. 100, p. 733–764), are reproduced here with improved color and resolution.


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  		FIG. 6. Photographs of different Na-Fe-Ca alteration styles and intensity in granite and comendite. Ja-30: Fresh, medium grained granite. Ja-25: Incipient fenitization with an aegirine vein and aegirine + albite clusters. Ja-28: Moderate fenitization with quartz dissolution near aegirine vein walls and strong albitization of feldspars. Ja-34: Swarm of subparallel and thin albite + aegirine + calcite . . . [Full Text of this Article]

 





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