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Sturm, Robert (2017) Cordierite from a high-temperature low-pressure shear zone of the south-western Bohemian Massif (Moldanubian terrain, Austria) Geochemistry, 77 (1) 195-206 doi:10.1016/j.chemer.2016.10.005

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Reference TypeJournal (article/letter/editorial)
TitleCordierite from a high-temperature low-pressure shear zone of the south-western Bohemian Massif (Moldanubian terrain, Austria)
JournalGeochemistry
AuthorsSturm, RobertAuthor
Year2017 (April)Volume77
Issue1
PublisherElsevier BV
DOIdoi:10.1016/j.chemer.2016.10.005Search in ResearchGate
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Mindat Ref. ID670900Long-form Identifiermindat:1:5:670900:0
GUID0
Full ReferenceSturm, Robert (2017) Cordierite from a high-temperature low-pressure shear zone of the south-western Bohemian Massif (Moldanubian terrain, Austria) Geochemistry, 77 (1) 195-206 doi:10.1016/j.chemer.2016.10.005
Plain TextSturm, Robert (2017) Cordierite from a high-temperature low-pressure shear zone of the south-western Bohemian Massif (Moldanubian terrain, Austria) Geochemistry, 77 (1) 195-206 doi:10.1016/j.chemer.2016.10.005
In(2017, April) Geochemistry Vol. 77 (1) Elsevier BV

See Also

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Sturm, Robert (2010) Morphology and growth trends of accessory zircons from various granitoids of the South-western Bohemian Massif (Moldanubicum, Austria) Geochemistry, 70 (2) 185-196 doi:10.1016/j.chemer.2009.05.001
CARSWELL, D. A., O'BRIEN, P. J. (1993) Thermobarometry and Geotectonic Significance of High-Pressure Granulites: Examples from the Moldanubian Zone of the Bohemian Massif in Lower Austria. Journal of Petrology, 34 (3) 427-459 doi:10.1093/petrology/34.3.427
Tropper, P., Deibl, I., Finger, F., Kaindl, R. (2006) P–T–t evolution of spinel–cordierite–garnet gneisses from the Sauwald Zone (Southern Bohemian Massif, Upper Austria): is there evidence for two independent late-Variscan low-P/high-T events in the Moldanubian Unit?. International Journal of Earth Sciences, 95 (6) 1019-1037 doi:10.1007/s00531-006-0082-x
KURAT, G, SCHARBERT, H (1972) Compositional zoning in garnets from granulite facies rocks of the Moldanubian Zone, Bohemian Massif of Lower Austria, Austria. Earth and Planetary Science Letters, 16 (3) 379-387 doi:10.1016/0012-821x(72)90155-0
Scharbert, H. G. (1973): Pyrope-rich garnets from Moldanubian garnet pyroxenites, Bohemian Massif, Lower Austria, Austria. N. Jb. Mineral. Mh., 1973, 80-83
Carswell, Dennis A. (1991) Variscan high P-T metamorphism and uplift history in the Moldanubian Zone of the Bohemian Massif in Lower Austria. European Journal of Mineralogy, 3 (2) 323-342 doi:10.1127/ejm/3/2/0323
Gebauer, D., Friedl, G. (1994) A 1.38 Ga protolith age for the Dobra orthogneiss (Moldanubian Zone of the southern Bohemian Massif, NE-Austria) Evidence from ion-microprobe (SHRIMP) dating of zircon. Journal of the Czech Geological Society, 39 (1) 34
Becker, H. (1994) Geochemistry of High-Temperature Garnet Peridotite Complexes from Lower Austria (Southern Bohemian Massif): Crustal Signatures in the Lower Lithosphere. Mineralogical Magazine, 58 (1) 67-68 doi:10.1180/minmag.1994.58a.1.38
Scharbert, Heinz G. (1973) Pyrope-rich garnets from Moldanubian garnet pyroxenites, Bohemian Massif of Lower Austria, Austria. Neues Jahrbuch fĂĽr Mineralogie - Monatshefte, 1973 (2). doi:10.1127/njmm/1973/1973/89
(1993) The Moldanubian/Saxothuringian Boundary at the Western Border of the Bohemian Massif - a Polyphase Strike-slip Zone. Zeitschrift der Deutschen Geologischen Gesellschaft, 144 (1) 68-87 doi:10.1127/zdgg/144/1993/68
Scharbert, Heinz G. (1973) Garnets from Moldanubian garnet pyroxenites and associated pyriclasites, Bohemian Massif of Lower Austria, Austria. Earth and Planetary Science Letters, 20 (3) 415-418 doi:10.1016/0012-821x(73)90019-8
 
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