Ti- and Zr-minerals in calcite-dolomite marbles from the ultrahigh-pressure 
Kimi Complex, Rhodope mountains, Greece: Implications for the P-T evolution 
based on reaction textures, petrogenetic grids, and geothermobarometry

Proyer, A.; Baziotis, I.; Mposkos, E.; Rhede, D.

doi:10.2138/am.2014.4710

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Ti- and Zr-minerals in calcite-dolomite marbles from the ultrahigh-pressure Kimi Complex, Rhodope mountains, Greece: Implications for the P-T evolution based on reaction textures, petrogenetic grids, and geothermobarometry

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Proyer, A.
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Baziotis, I.
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Mposkos, E.
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Rhede, D.
4.2 Inorganic and Isotope Geochemistry, 4.0 Chemistry and Material Cycles, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Proyer, A., Baziotis, I., Mposkos, E., Rhede, D. (2014): Ti- and Zr-minerals in calcite-dolomite marbles from the ultrahigh-pressure Kimi Complex, Rhodope mountains, Greece: Implications for the P-T evolution based on reaction textures, petrogenetic grids, and geothermobarometry. - American Mineralogist, 99, 7, 1429-1448.
https://doi.org/10.2138/am.2014.4710

Cite as: https://gfzpublic.gfz.de/pubman/item/item_691904

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