Genesis of amethyst geodes in basaltic rocks of the Serra Geral Formation (Ametista do Sul, Rio Grande do Sul, Brazil): a fluid inclusion, REE, oxygen, carbon, and Sr isotope study on basalt, quartz, and calcite

Gilg, H. Albert; Morteani, Giulio; Kostitsyn, Yuri A.; Preinfalk, Christine; Gatter, István; Strieder, Adelir J.

doi:10.1007/s00126-002-0310-7

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Genesis of amethyst geodes in basaltic rocks of the Serra Geral Formation (Ametista do Sul, Rio Grande do Sul, Brazil): a fluid inclusion, REE, oxygen, carbon, and Sr isotope study on basalt, quartz, and calcite

Author(s): H. Albert Gilg , Giulio Morteani , Yuri Kostitsyn , Christine Preinfalk , Istvan Gatter , Adelir J. Strieder

Publication date (Electronic): August 27 2002

Journal: Mineralium Deposita

Publisher: Springer Science and Business Media LLC

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Most cited references 46

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The stable isotopic composition of modern soil carbonate and its relationship to climate

Thure E. Cerling (1984)

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Oxygen isotope exchange between quartz and water

Robert Clayton, Toshiko Mayeda, James R. O'Neil (1972)

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Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

Michael Bau (1991)

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Journal

Title: Mineralium Deposita

Abbreviated Title: Miner Deposita

Publisher: Springer Science and Business Media LLC

ISSN (Print): 0026-4598

ISSN (Electronic): 1432-1866

Publication date Created: December 2003

Publication date (Electronic): August 27 2002

Publication date (Print): December 2003

Volume: 38

Issue: 8

Pages: 1009-1025

Article

DOI: 10.1007/s00126-002-0310-7

SO-VID: d5f3863a-f6eb-4d22-bf30-ebc1b229c008

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Genesis of amethyst geodes in basaltic rocks of the Serra Geral Formation (Ametista do Sul, Rio Grande do Sul, Brazil): a fluid inclusion, REE, oxygen, carbon, and Sr isotope study on basalt, quartz, and calcite

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Most cited references 46

The stable isotopic composition of modern soil carbonate and its relationship to climate

Oxygen isotope exchange between quartz and water

Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

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