Rooseveltite from San Francisco de los Andes and Cerro Negro de la Aguadita, San Juan, Argentina

Rooseveltite occurs in the weathering zone of the San Francisco de los Andes and Cerro Negro de la Aguadita mines, located in the San Juan Province, Argentina, at 30° 22′S and 69° 33′W. It appears in grey, finegrained aggregates pseudomorph after bismuthinite. Refraction index ranges from n=2.10 to...

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Autor principal: Bedlivy, D.
Otros Autores: Llambías, E.J, Astarloa, J.F.H
Formato: Capítulo de libro
Lenguaje:Alemán
Publicado: Springer-Verlag 1972
Acceso en línea:Registro en Scopus
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100 1 |a Bedlivy, D. 
245 1 0 |a Rooseveltite from San Francisco de los Andes and Cerro Negro de la Aguadita, San Juan, Argentina 
246 3 1 |a Rooseveltit von San Francisco de los Andes und Cerro Negro de la Aguadita, San Juan, Argentinien 
260 |b Springer-Verlag  |c 1972 
270 1 0 |m Bedlivy, D.; Dpt. Cs. Geológicas, Fac. Cs. Exactes y Naturales, Univ. Buenos Aires, Ciudad Universitaria Pabellón 2, Buenos Aires, Argentina 
506 |2 openaire  |e Política editorial 
504 |a Bedlivy, D., Llambías, E.J., Cu-, Fe- und Pb-Arsenate von San Francisco de los Andes, Provinz San Juan, Argentinien (1969) (Spanisch.) Rev. Asoc. Geol. Arg., 24, pp. 29-40 
504 |a Bedlivy, D., Llambías, E.J., Astarloa, J., Wismutarsenate von San Francisco de los Andes und Cerro Negro de la Aguadita, San Juan, Argentinien. (Spanisch.) 4 (1969) Jornadas Geol. Argentinas, 1, pp. 67-73 
504 |a Boyle, R. W., 1965: Geology, Geochemistry and origin of the lead-zinc-silver deposits of the Keno Hill-galena Hill area, Yukon Territory, Geol. Surv. Canada, Bull. 111; Evans, H. T., Jr., D. E. Appleman, and D. S. Handwerker, 1963: The least-squares refinement of crystal unit cells with power diffraction by an automatic computer indexing method (abstr.). Amer Crystallogr. Assoc., Cambridge, Mass., Ann. Meet. Program, 42–43; Frondel, C., New data on agricolite, bismoclite, koechlinite and the bismuth arsenates (1943) Amer. Min., 28, pp. 536-540 
504 |a Frondel, C., (1951) Dana's System of Mineralogy, p. 697. , Wiley, New York-London 
504 |a Garrels, R.M., Mineral species as functions of pH and oxidation-reduction potentials, with special reference to the zone of oxidation and secondary enrichment, of sulfide ore desposits (1954) Geochim. Cosmochim. Acta, 5, pp. 153-168 
504 |a Gmelins, (1964) Handbuch der anorg, p. 631. , Chemie, System, Nr. 19, Verlag Chemie., Weinheim/Bergstr 
504 |a Herzenberg, R., Neue Minerale Boliviens (1946) (Spanisch.) Bol. Técnico, Facultad Nac. Ing., Univ. Técnica de Oruro, 1, pp. 10-11 
504 |a Llambías, E.J., Malvicini, L., Die mit den granitischen Plutonen der Cordillera Frontal verbundenen Metallogenese zwischen dem Tal von Agua Negra und Rio Castano, San Juan, Argentinien (1966) (Spanisch.) Rev. Asoc. Geol. Arg., 21, pp. 239-261 
504 |a Llambías, E.J., Malvicini, L., The geology and genesis of the Bi−Cu mineralized breccia-pipe, San Francisco de los Andes, San Juan, Argentina (1969) Econ. Geol., 64, pp. 271-286 
504 |a Mooney, R.C.L., Crystal structure of tetragonal, bismuth arsenate, BiAsO<inf>4</inf> (1948) Acta Crystallographica, 1, pp. 163-165 
504 |a Mooney-Slater, R.C.L., Polymorphic forms of bismuth phosphate (1962) Z. Krist., 117, p. 378 
504 |a Pabst, A., Huttonite a new monoclinic thorium silicate (1951) Amer. Min., 36, p. 60 
504 |a Rosenheim, A., Thon, A., Über die Komplexbildung des Arsenatanions (1927) Z. anorg. allg., Chem., 167 (10), p. 14 
504 |a Sato, M., Oxidation of sulfide ore bodies. II. Oxidation mechanisms of sulfide minerals at 25°C (1960) Econ. Geol., 55, p. 1202 
504 |a de Schulten, A., Phosphate et arséniate de bismuth (1903) Bull. Soc. chim. France [3], 29, p. 724 
504 |a Schwarz, H., Die Phosphate, Arsenate und Vanadate der Seltenen Erden (1963) Z. anorg. allg. Chem., 323, pp. 52-56 
520 3 |a Rooseveltite occurs in the weathering zone of the San Francisco de los Andes and Cerro Negro de la Aguadita mines, located in the San Juan Province, Argentina, at 30° 22′S and 69° 33′W. It appears in grey, finegrained aggregates pseudomorph after bismuthinite. Refraction index ranges from n=2.10 to 2.30. The Vickers microhardness is 513 (4-5 of Mohs' scale). Chemical composition from electron micro probe measurements is As 21.5±1% and Bi 60.9±2%. Rooseveltite is monoclinic, with a0=6.878(1) Å, b0=7.163(1) Å, c0=6.735(1) Å, β=104° 46′±1′, Z=4, ρcalc.=6,94 g·cm-3, space group P 21/n. The synthetic compound was prepared by three different methods. The powder pattern are the same as that of the mineral. Refraction index nα=2.13(2) and nγ=2.25(2). The measured specific gravity is ρpobs.=7,01 g·cm-3. Cell parameters: a0=6.882(1) Å, b0=7.164(1) Å, c0=6.734(1) Å, β=104° 50.5′±0.7′, ρcalc.=6,94 g·cm-3. The synthetic material melts at about 950°C. After heating to 920°C no variations were observed in the powder diagram of the mineral. It is tried to explain the formation of rooseveltite in natural environment. © 1972 Springer-Verlag.  |l eng 
593 |a Dpt. Cs. Geológicas, Fac. Cs. Exactes y Naturales, Univ. Buenos Aires, Ciudad Universitaria Pabellón 2, Buenos Aires, Argentina 
593 |a Univ. Nacional del Sur, Bahía Blanca, Argentina 
700 1 |a Llambías, E.J. 
700 1 |a Astarloa, J.F.H. 
773 0 |d Springer-Verlag, 1972  |g v. 17  |h pp. 65-75  |k n. 2  |p TMPM Tschermaks Petr. Mitt.  |x 00413763  |t TMPM Tschermaks Mineralogische und Petrographische Mitteilungen 
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