Evolution of a Cambro-Ordovician active margin in northern Gondwana: Geochemical and zircon geochronological evidence from the Góry Sowie metasedimentary rocks, Poland-Reference-Cited by-同舟云学术

Evolution of a Cambro-Ordovician active margin in northern Gondwana: Geochemical and zircon geochronological evidence from the Góry Sowie metasedimentary rocks, Poland

Published:2021-02 Issue: Volume:90 Page:1-26
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Tabaud A.S.,Štípská P.,Mazur S.,Schulmann K.,Míková J.,Wong J.,Sun M.

Funder

Česká geologická služba

Grantová Agentura České Republiky

Publisher

Elsevier BV

Subject

Geology

Reference171 articles.

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4. Experimental study of zircon coarsening in quartzite ± H2O at 1.0 GPa and 1000 °C, with implications for geochronological studies of high-grade metamorphism;Ayers;Am. Mineral.,2003

5. Mineral chemistry of garnet lherzolites from the Sudetes, Southwest Poland;Bakun-Czubarow;Carnegie Inst. Wash. Yearb.,1983

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