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Genesis of the Silvermines zinc-lead-barite deposit, Ireland; fluid inclusion and stable isotope evidence

Economic Geology (1987) 82 (2): 371–394.
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Anomalously Metal-Rich Fluids Form Hydrothermal Ore Deposits
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Reply to the comments by Marignac and Cathelineau on the paper by Sánchez-España et al.: Source and evolution of ore-forming hydrothermal fluids in the northern Iberian Pyrite Belt massive sulphide deposits (SW Spain): evidence from fluid inclusions and stable isotopes (Mineralium Deposita 38: 519–537)
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Mineralium Deposita (2006) 40 (6-7): 749.
Metal sources of the Navan carbonate-hosted base metal deposit, Ireland: Nd and Sr isotope evidence for deep hydrothermal convection
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Mineralium Deposita (2006) 41 (8): 803.
Environment of formation and styles of volcanogenic massive sulfides: The Iberian Pyrite Belt
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Stable Isotope Geochemistry of the Carboniferous Zn-Pb-Cu Sediment-Hosted Sulfide Deposits, Northeastern Spain
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Lower Carboniferous peritidal carbonates and associated evaporites adjacent to the Leinster Massif, southeast Irish Midlands
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Irish Lower Carboniferous replacement dolomite: isotopic modelling evidence for a diagenetic origin involving low-temperature modified seawater
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Geological Society, London, Special Publications (2004) 235 (1): 75.
Metamorphic and basin fluids in quartz–carbonate–sulphide veins in the SW Scottish Highlands: a stable isotope and fluid inclusion study
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On diagenesis, dolomitisation and mineralisation in the Irish Zn-Pb orefield
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Mineralium Deposita (2003) 38 (8): 968.
Origin and migration of fluids during the evolution of sedimentary basins and the origin of ZnPb deposits in Western and Central Europe
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A mineralogical and fluid inclusion study of the Harberton Bridge Fe–Zn–Pb deposit, County Kildare, Ireland
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The Importance of Oxidized Brines for the Formation of Australian Proterozoic Stratiform Sediment-Hosted Pb-Zn (Sedex) Deposits
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