Faryad, Shah Wali (2009) The Kutná Hora Complex (Moldanubian zone, Bohemian Massif): A composite of crustal and mantle rocks subducted to HP/UHP conditions. Lithos, 109 (3) 193-208 doi:10.1016/j.lithos.2008.03.005
Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | The Kutná Hora Complex (Moldanubian zone, Bohemian Massif): A composite of crustal and mantle rocks subducted to HP/UHP conditions | ||
Journal | Lithos | ||
Authors | Faryad, Shah Wali | Author | |
Year | 2009 (May) | Volume | 109 |
Page(s) | 193-208 | Issue | 3 |
Publisher | Elsevier BV | ||
DOI | doi:10.1016/j.lithos.2008.03.005Search in ResearchGate | ||
Mindat Ref. ID | 271506 | Long-form Identifier | mindat:1:5:271506:7 |
GUID | 095e01e6-fb6d-407c-9d23-383b6b242708 | ||
Full Reference | Faryad, Shah Wali (2009) The Kutná Hora Complex (Moldanubian zone, Bohemian Massif): A composite of crustal and mantle rocks subducted to HP/UHP conditions. Lithos, 109 (3) 193-208 doi:10.1016/j.lithos.2008.03.005 | ||
Plain Text | Faryad, Shah Wali (2009) The Kutná Hora Complex (Moldanubian zone, Bohemian Massif): A composite of crustal and mantle rocks subducted to HP/UHP conditions. Lithos, 109 (3) 193-208 doi:10.1016/j.lithos.2008.03.005 | ||
In | (2009, May) Lithos Vol. 109 (3) Elsevier BV |
References Listed
These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
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Not Yet Imported: Journal of GEOsciences - journal-article : 10.3190/JCGS.980 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 42404 | |
Zhang, R.Y., Yang, J.S., Wooden, J.L., Liou, J.G., Li, T.F. (2005) U–Pb SHRIMP geochronology of zircon in garnet peridotite from the Sulu UHP terrane, China: Implications for mantle metasomatism and subduction-zone UHP metamorphism. Earth and Planetary Science Letters, 237 (3) 729-743 doi:10.1016/j.epsl.2005.07.003 |
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