(PDF) The Chemical Evolution From Older (323

The Chemical Evolution From Older (323–318 Ma) Towards Younger Highly Evolved Tin Granites (315–314 Ma)—sources and Metal Enrichment in Variscan Granites of the Western Erzgebirge (Central European Variscides, Germany)

doi 10.5194/egusphere-egu2020-3092

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March 9, 2020

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The Chemical Evolution From Older (323&#8211;318 Ma) Towards Younger Highly Evolved Tin Granites (315&#8211;314 Ma)&#8212;sources and Metal Enrichment in Variscan Granites of the Western Erzgebirge (Central European Variscides, Germany)

doi 10.5194/egusphere-egu2020-3092

Full Text

Abstract

Date

Authors

Publisher

Related search

The Rare Earth Elements Geochemistry of Lingshan Tungsten-Tin-Bearing Granites and Their Applications to Petrogenesis of the Granites

Geochemical and Isotopic (Sr, Nd and O) Constraints on Sources for Variscan Granites in the Western Carpathians - Implications for Crustal Structure and Tectonics

Magnetic Mineralogy of Variscan Granites From Northern Portugal: An Approach to Their Petrogenesis and Metallogenic Potential.

Rare Metal Granites and Related Rocks of the Ukrainian Shield

U-Pb Zircon Age of the Youngest Magmatic Activity in the High Tatra Granites (Central Western Carpathians)

The Geochemistry of Biotites From Granites of Northern Portugal With Special Reference to Their Tin Content

Zircon Perspectives on the Age and Origin of Evolved S-Type Granites From the Cornubian Batholith, Southwest England

Rare Metal Mineralization of Tin Manifestations in the Area of Lithium-Fluoric Granites (Verkhneurmiysk Ore Cluster, the Amur River Region)

The Evolution of Late-Hercynian Granites and Rhyolites Documented by Quartz – A Review

The Chemical Evolution From Older (323–318 Ma) Towards Younger Highly Evolved Tin Granites (315–314 Ma)—sources and Metal Enrichment in Variscan Granites of the Western Erzgebirge (Central European Variscides, Germany)