2013
DOI: 10.1016/j.oregeorev.2012.08.001
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Evolution of unconformity-related MnFeAs vein mineralization, Sailauf (Germany): Insight from major and trace elements in oxide and carbonate minerals

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Cited by 15 publications
(2 citation statements)
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“…The composition of trace elements in groundwater is determined by mineral dissolution and several geochemical processes. Trace elements can be mainly contained in silicates, but also, they can be associated to carbonate and evaporite minerals (Dean 1978 ; Fusswinkel et al 2013 ). However, trace element concentrations in groundwater are controlled by several processes such as surface sorption/desorption, ion exchange, precipitation/dissolution, chelation, and microbial removal/input (Leung and Jiao 2006 ).…”
Section: Discussionmentioning
confidence: 99%
“…The composition of trace elements in groundwater is determined by mineral dissolution and several geochemical processes. Trace elements can be mainly contained in silicates, but also, they can be associated to carbonate and evaporite minerals (Dean 1978 ; Fusswinkel et al 2013 ). However, trace element concentrations in groundwater are controlled by several processes such as surface sorption/desorption, ion exchange, precipitation/dissolution, chelation, and microbial removal/input (Leung and Jiao 2006 ).…”
Section: Discussionmentioning
confidence: 99%
“…In the field, it is difficult to distinguish calcite that formed during the syn-ore and barren stages in terms of texture and colour, especially given the local occurrence of cinnabar in the veins. However, the trace element and isotopic compositions of calcite may contain information about the oreforming fluids and can be used to constrain its origin (Fusswinkel et al, 2013;Smith-Schmitz and Appold, 2018). The two stages of hydrothermal calcite identified in the Jianyan Hg deposit have similar Fe but variable Mn contents (Figure 5a).…”
Section: Differentiation Of Calcite Of the Syn-ore And Barren Stages ...mentioning
confidence: 99%