Diamond and coesite inclusions in detrital garnet of the Saxonian Erzgebirge, Germany
Author:
Affiliation:
1. Geoscience Center Göttingen, University of Göttingen, Goldschmidtstraße 3, 37077 Göttingen, Germany
2. School of Geography, Geology and the Environment, Keele University, Keele, Staffordshire ST5 5BG, UK
Abstract
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/geology/article-pdf/doi/10.1130/G46253.1/4708101/g46253.pdf
Reference19 articles.
1. How geometry and anisotropy affect residual strain in host-inclusion systems: Coupling experimental and numerical approaches;Campomenosi;American Mineralogist,2018
2. First find of polycrystalline diamond in ultrahigh-pressure metamorphic terrane of Erzgebirge, Germany;Dobrzhinetskaya;Journal of Metamorphic Geology,2013
3. Micropetrology: Are inclusions grains of truth?;Ferrero;Journal of Petrology,2018
4. Raman mapping of coesite inclusions in garnet from the Kokchetav Massif (Northern Kazakhstan): Spectrochimica Acta, Part A;Korsakov;Molecular and Biomolecular Spectroscopy,2007
5. Diamond and coesite discovered in Saxony-type granulite: Solution to the Variscan garnet peridotite enigma;Kotková;Geology,2011
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