Trace Element Geochemistry of Alluvial TiO2 Polymorphs as a Proxy for Sn and W Deposits

The Segura mining field, the easternmost segment of the Góis–Panasqueira–Segura tin– tungsten metallogenic belt (north–central Portugal), includes Sn-W quartz veins and Li-Sn aplitepegmatites, which are believed to be genetically related to Variscan Granites. Sediment geochemistry indicates granite-...

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Bibliographic Details
Main Author: Gaspar, Miguel (author)
Other Authors: Grácio, Nuno (author), Salgueiro, Rute (author), Costa, Mafalda (author)
Format: article
Language:eng
Published: 2022
Subjects:
TiO2 polymorphs
alluvial
heavy minerals
Sn-W deposits
trace elements
geochemical footprints
geochemical fingerprints
geochemical exploration
Online Access:http://hdl.handle.net/10174/32582
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/32582

Internet

http://hdl.handle.net/10174/32582

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