Tichomirowa, M.; Gerdes, A.; Lapp, M.; Leonhardt, D.; Whitehouse, M.
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). Minerals 2019, 9, 769.
https://doi.org/10.3390/min9120769
AMA Style
Tichomirowa M, Gerdes A, Lapp M, Leonhardt D, Whitehouse M.
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). Minerals. 2019; 9(12):769.
https://doi.org/10.3390/min9120769
Chicago/Turabian Style
Tichomirowa, Marion, Axel Gerdes, Manuel Lapp, Dietmar Leonhardt, and Martin Whitehouse.
2019. "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)" Minerals 9, no. 12: 769.
https://doi.org/10.3390/min9120769
APA Style
Tichomirowa, M., Gerdes, A., Lapp, M., Leonhardt, D., & Whitehouse, M.
(2019). 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). Minerals, 9(12), 769.
https://doi.org/10.3390/min9120769