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Two-phase late Paleozoic magmatism (~ 313–312 and ~ 299–298 Ma) in the Lusatian Block and its relation to large scale NW striking fault zones: evidence from zircon U–Pb CA–ID–TIMS geochronology, bulk rock- and zircon chemistry
ORCID iD: 0000-0002-2566-7747
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2021 (English)In: International journal of earth sciences, ISSN 1437-3254, E-ISSN 1437-3262, Vol. 110, no 8, p. 2923-2953Article in journal (Refereed) Published
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2021. Vol. 110, no 8, p. 2923-2953
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Geochemistry
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The changing Earth
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URN: urn:nbn:se:nrm:diva-4694DOI: 10.1007/s00531-021-02092-yOAI: oai:DiVA.org:nrm-4694DiVA, id: diva2:1622486
Available from: 2021-12-22 Created: 2021-12-22 Last updated: 2021-12-22Bibliographically approved

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Käßner, A.Whitehouse, Martin J.
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