El origen del azufre en mineralizaciones filonianas en el centra de la Península Ibérica

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El-origen.pdf (279.77 KB)

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1995

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http://hdl.handle.net/10272/13389

Abstract

Sulphur isotope data from several base metals-Ba-(F)-(Ag) and Ag-base metals vein-type deposits in the Central Iberian Zone o f the Hesperian Massif suggest a magmatic and /or metasedimentary origin o f this ore-forming component. Deposits exclusively hosted in metasediments (p.e. Alcudia Valley, type IV) display a magmatic signature. Even those lodes and stratabound deposits hosted by Permian-Triassic terrigenous and andesites (Las Torrecillas-Linares y Atienza) are formed by "igneous" sulphur

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Pb-Zn; Ag; Vein-type mineralizations; Spanish Central System; Linares-La Carolina; Alcudia Valley; Central Iberian Zone

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Geogaceta -- Nº 19, (1995)
Atribución-NoComercial-SinDerivadas 3.0 España
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España