Contrasting coronas: microscale fluid variation deduced from monazite breakdown products in altered metavolcanic rocks associated with the Grängesberg apatite-iron oxide ore, Bergslagen, Sweden-Reference-Cited by-同舟云学术

Contrasting coronas: microscale fluid variation deduced from monazite breakdown products in altered metavolcanic rocks associated with the Grängesberg apatite-iron oxide ore, Bergslagen, Sweden

Published:2022-04-03 Issue:2 Volume:144 Page:89-96
ISSN:1103-5897
Container-title:GFF
language:en
Short-container-title:GFF

Author:

Majka Jarosław¹²^ORCID,Włodek Adam²^ORCID,Jonsson Erik¹³,Högdahl Karin¹^ORCID

Affiliation:

1. Department of Earth Sciences, Uppsala University, Uppsala, Sweden

2. Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Kraków, Poland

3. Department of Mineral Resources, Geological Survey of Sweden, Uppsala, Sweden

Funder

Geological Survey of Sweden

AGH-UST

Publisher

Informa UK Limited

Subject

Paleontology,Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/11035897.2022.2083224

Reference24 articles.

1. Facies analysis of a 1.9 Ga, continental margin, back-arc, felsic caldera province with diverse Zn-Pb-Ag-(Cu-Au) sulfide and Fe oxide deposits, Bergslagen region, Sweden

2. Redistribution of rare earth elements, thorium, and uranium over accessory minerals in the course of amphibolite to granulite facies metamorphism: The role of apatite and monazite in orthogneisses from southwestern Norway

3. Alteration and breakdown of xenotime-(Y) and monazite-(Ce) in granitic rocks of the Western Carpathians, Slovakia

4. Experimental constraints on the relative stabilities of the two systems monazite-(Ce) – allanite-(Ce) – fluorapatite and xenotime-(Y) – (Y,HREE)-rich epidote – (Y,HREE)-rich fluorapatite, in high Ca and Na-Ca environments under P-T conditions of 200–1000 MPa and 450–750 °C

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