| dc.creator | Monteiro L.V.S. | |
| dc.creator | Xavier R.P. | |
| dc.creator | Hitzman M.W. | |
| dc.creator | Juliani C. | |
| dc.creator | de Souza Filho C.R. | |
| dc.creator | Carvalho E.d.R. | |
| dc.date | 2008 | |
| dc.date | 2015-06-30T19:29:30Z | |
| dc.date | 2015-11-26T14:44:50Z | |
| dc.date | 2015-06-30T19:29:30Z | |
| dc.date | 2015-11-26T14:44:50Z | |
| dc.date.accessioned | 2018-03-28T21:53:51Z | |
| dc.date.available | 2018-03-28T21:53:51Z | |
| dc.identifier | | |
| dc.identifier | Ore Geology Reviews. , v. 34, n. 3, p. 317 - 336, 2008. | |
| dc.identifier | 1691368 | |
| dc.identifier | 10.1016/j.oregeorev.2008.01.003 | |
| dc.identifier | http://www.scopus.com/inward/record.url?eid=2-s2.0-53349127862&partnerID=40&md5=3c38576efeebe87c6bc12696d2fc4e35 | |
| dc.identifier | http://www.repositorio.unicamp.br/handle/REPOSIP/106450 | |
| dc.identifier | http://repositorio.unicamp.br/jspui/handle/REPOSIP/106450 | |
| dc.identifier | 2-s2.0-53349127862 | |
| dc.identifier.uri | http://repositorioslatinoamericanos.uchile.cl/handle/2250/1252276 | |
| dc.description | The Sossego iron oxide-copper-gold deposit in the Carajás Mineral Province comprises two major orebodies, Sequeirinho and Sossego. Sodic alteration (albite-hematite) and sodic-calcic alteration zones represented by albite, ferro-edenite/hastingsite (up to 3.8 wt.% Cl), actinolite/magnesiohornblende, magnetite, titanite, epidote, and calcite are predominant at Sequeirinho. Magnetite bodies with envelopes of apatite-rich actinolitite were formed with the sodic-calcic event at high temperatures (~ 500 °C at 1.4 kbar). In the Sossego orebody, potassic alteration with orthoclase and Cl-rich biotite (up to 3.1 wt.%) and chloritization are the main alteration types. Mineralized breccias in both orebodies have coarse-grained zoned actinolite/ferro-actinolite, Cl-apatite, and magnetite within the matrix. Sulfides occur in equilibrium with a paragenetically late calcite-quartz-chlorite-epidote-allanite assemblage. The AlIV contents of the chlorite indicate crystallization at temperatures below 300 °C. Chalcopyrite occurs associated with pyrite (up to 2.3 wt.% Co and 0.2 wt.% Ni), native gold (up to 14.9 wt.% Ag), siegenite, millerite, vaesite, Pd-melonite, and hessite. Dilution and cooling of the hot metalliferous fluid (> 500 °C) by mixing with meteoric fluids may have been the main mechanisms responsible for the deposition of metals transported as metal chloride complexes in both orebodies of the Sossego deposit. © 2008 Elsevier B.V. All rights reserved. | |
| dc.description | 34 | |
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| dc.description | 336 | |
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| dc.language | en | |
| dc.publisher | | |
| dc.relation | Ore Geology Reviews | |
| dc.rights | fechado | |
| dc.source | Scopus | |
| dc.title | Mineral Chemistry Of Ore And Hydrothermal Alteration At The Sossego Iron Oxide-copper-gold Deposit, Carajás Mineral Province, Brazil | |
| dc.type | Artículos de revistas | |
