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1.- AN EXPLANATION FOR THE ORIGIN OF HEMIHEDRISM IN WULFENITE; THE SINGLE-CRYSTAL STRUCTURES OF (SUB 1) /A AND IOTA 4TUNGSTENIAN WULFENITES
MINERALOGICAL SOCIETY; LONDON; GBR; UNITED KINGDOM, 2000
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2.- Paratacamite-(Mg), Cu (sub 3) (Mg,Cu)Cl (sub 2) (OH) (sub 6) ; a new substituted basic copper chloride mineral from Camerones, Chile
Mineralogical Society; London; GBR; United Kingdom, 2013
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