2011
DOI: 10.2113/econgeo.106.7.1111
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The Lagoa Salgada Orebody, Iberian Pyrite Belt, Portugal

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Cited by 30 publications
(26 citation statements)
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“…These two rhyodacites are clearly distinguished by their phenocryst content; geochemically, the former corresponds to a more evolved series than the latter. The Central Stockwork is characterized by minor Pb, Zn and Sn, and Cu values can reach 1.4 wt % [11].…”
Section: The Lagoa Salgada Orebodymentioning
confidence: 99%
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“…These two rhyodacites are clearly distinguished by their phenocryst content; geochemically, the former corresponds to a more evolved series than the latter. The Central Stockwork is characterized by minor Pb, Zn and Sn, and Cu values can reach 1.4 wt % [11].…”
Section: The Lagoa Salgada Orebodymentioning
confidence: 99%
“…Setting Lagoa Salgada aside from other nearby VHMS deposits is the presence of indium as a trace element within the base metal element suite. This very scarce metal is preferentially hosted by sphalerite (see Figure 10 from [11]), with contents attaining an average maximum of 0.62% In. The fact that until now discrete inclusions of In-bearing minerals have not been observed reinforces the idea that indium occurs possibly within nanophases [12] as postulated before [1].…”
Section: The Lagoa Salgada Orebodymentioning
confidence: 99%
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“…Major In deposits or mineralization regions have been identified throughout the world, such as Mount Pleasant in Canada [6][7][8], southwestern Bolivia [4,9], southern Finland and adjacent areas [10][11][12], southwestern England [13], the eastern Erzgebirge in Germany [14], the Iberian Pyrite Belt [15,16], Japanese Arc [5,17], the Southern Dahinggang Mountains in northern China [18,19], and southern China [20][21][22][23][24]. Two types of primary, industrial In-bearing deposits have been identified: (1) volcanic-hosted massive sulfide deposits, e.g., Kidd Creek in Canada and Neves Corvo in The Xianghualing Orefield is a typical Sn-ploymetallic orefield in southern Hunan.…”
Section: Introductionmentioning
confidence: 99%
“…Although In occurs mainly in an isomorphic form in sphalerite, important resources are hosted in Sn-rich deposits. Examples include Sn-polymetallic deposits in south China [5][6][7], Bolivia [8], Japan [2,4], and some Sn-rich Cu-Zn deposits within the Iberian Pyrite Belt [9][10][11] and the Meng'entaolegai Ag-Pb-Zn deposit in north China [12]. Considering these associations with Sn-rich mineralization, could In-rich deposits also occur in Sn-poor environments?…”
Section: Introductionmentioning
confidence: 99%