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Transport and fixation of arsenic in geothermal eviroments - a case study of the fossil geothermal system at Sailauf

Fachliche Zuordnung Mineralogie, Petrologie und Geochemie
Förderung Förderung von 2008 bis 2013
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 61069113
 
Erstellungsjahr 2014

Zusammenfassung der Projektergebnisse

Quantitative understanding of element mobility in hydrothermal systems and the underlying ore forming processes requires in-depth knowledge about mineralogy, mineral chemistry and fluid geochemistry. We report results of an integrated mineralogical and geochemical study of the unconformity-related hydrothermal Mn-Fe-As mineralization at Sailauf (Spessart, Germany). Combining detailed mineralogical and mineral chemical studies with in situ LA-ICPMS fluid inclusion spot analysis enabled reconstruction of a protracted post-Variscan fluid flow system encompassing mixing processes between red bed- and basement-interacted fluids with formation fluids derived from the overlying sedimentary sequence. Such mixing processes are commonly invoked to have facilitated formation of many different ore deposit types, yet their physical feasibility on the scale of individual ore veins is still disputed. Recent analytical advances in LA- ICPMS analysis of halogens (Cl/Br) in fluid inclusions provided the opportunity to study these processes in texturally well-constrainable fluid inclusion assemblages in a post-Variscan Pb-Znquartz vein deposit in the Schwarzwald district (Germany). For the first time, it was possible to clearly identify mixing processes on the mm-scale on growth zones of individual quartz crystals.

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