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Trace element geochemistry of sphalerite in contrasting hydrothermal fluid systems of the Freiberg d...

Trace element geochemistry of sphalerite in contrasting hydrothermal fluid systems of the Freiberg d...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2137401443

Trace element geochemistry of sphalerite in contrasting hydrothermal fluid systems of the Freiberg district, Germany: insights from LA-ICP-MS analysis, near-infrared light microthermometry of sphalerite-hosted fluid inclusions, and sulfur isotope geochemistry

About this item

Full title

Trace element geochemistry of sphalerite in contrasting hydrothermal fluid systems of the Freiberg district, Germany: insights from LA-ICP-MS analysis, near-infrared light microthermometry of sphalerite-hosted fluid inclusions, and sulfur isotope geochemistry

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

Journal title

Mineralium deposita, 2019-02, Vol.54 (2), p.237-262

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

More information

Scope and Contents

Contents

The historic silver mining district of Freiberg (Germany) comprises hydrothermal vein-style mineralization of Permian and Cretaceous age. We compare sphalerite compositions with associated ore-forming fluids and constrain the behavior of critical metals such as In, Ge, and Ga in contrasting hydrothermal environments. Fluid inclusion studies reveal...

Alternative Titles

Full title

Trace element geochemistry of sphalerite in contrasting hydrothermal fluid systems of the Freiberg district, Germany: insights from LA-ICP-MS analysis, near-infrared light microthermometry of sphalerite-hosted fluid inclusions, and sulfur isotope geochemistry

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2137401443

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2137401443

Other Identifiers

ISSN

0026-4598

E-ISSN

1432-1866

DOI

10.1007/s00126-018-0850-0

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