Hydrothermal Tourmaline from the Girvas Paleovolcano (Onega basin, Karelian Craton): Morphology and Chemical Composition

Author:

Svetova E. N.,Svetov S. A.

Publisher

Springer International Publishing

Reference10 articles.

1. Bychkov, A.Y., Popova, Y.A., Kivadze, O.E., Lubnina, N.V.: A thermodynamic model of chemical remagnetization based on the example of the Girvas Paleovolcano in the onega structure of the Carelian Craton. Moscow Univ. Geol. Bull.74,154–161 (2019)

2. Clark, K.M.: Tourmaline: structural formula calculations. Canadian Mineralogist. 45, 229−237 ( 2007)

3. Dutrow, B.L., Henry, D.J.: Tourmaline: a geologic DVD. Elements. 7, 301–306 (2011)

4. Field guidebook of XII all-Russian petrographic conference «Petrography of igneous and metamorphic rocks». Petrozavodsk: KRC RAS, p. 96 (2015). [In Russian]

5. Glushanin, L.V., Sharov, N.V., Shchiptsov, V.V.: Paleoproterozoic Onega structure: geology, tectonics, structure, and metallogeny; karelian research centre, RAS: Petrozavodsk, Russia, p. 431 (2011). (In Russian)

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