REE data of hydrothermal fluorite from the Finstergrund & Tannenboden veins (Wieden district, Black Forest, Germany)
DOI:
10.12297/dpr.dde.202305.1
Category:
C_CC_8_17C_CC_8_15C_CC_8_10
Keywords:
FluoriteREEFluid-rock interactionBlack Forest
Abstract
Dataset to Hintzen et al. (2023): Multistage fluorite mineralization in the southern Black
Forest, Germany: evidence from rare earth element (REE) geochemistry, published in European Journal of Mineralogy
The Black Forest hosts a wide range of hydrothermal mineralization, including fluorite–barite
vein deposits. In a detailed investigation of the Finstergrund and Tannenboden deposits in the Wieden mining district (southern Black Forest), the diversity, geochemical evolution and relative chronology of multistage fluorite precipitation is tracked on the basis of rare earth element (REE) geochemistry, geologic field relationships and crystal zoning. Geochemical discrimination and mathematical lambda coefficients suggest a total of seven fluorite
REE groups, at least three distinguishable post-Variscan fluid mobilization events and independent formation histories for the deposits despite their spatial proximity. The local diversity of REE patterns emphasizes the need for detailed investigations of individual hydrothermal vein deposits.
Entity Data
Fluorite_Finstergrund_Tannenboden_PAAS-norm-dataset_Hintzen et al.xlsx
Fluorite_Finstergrund_Tannenboden_LA-ICP-MS_Glitter_raw-data_Hintzen et al.xlsx
Reference This Dataset
Robin Hintzen.REE data of hydrothermal fluorite from the Finstergrund & Tannenboden veins (Wieden district, Black Forest, Germany).DDE Repository.2023-05-28.doi:10.12297/dpr.dde.202305.1