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Pomonis, Panagiotis, Magganas, Andreas (2017) Petrogenetic Implications for Ophiolite Ultramafic Bodies from Lokris and Beotia (Central Greece) Based on Chemistry of Their Cr-spinels. Geosciences, 7 (1) 10 doi:10.3390/geosciences7010010

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Reference TypeJournal (article/letter/editorial)
TitlePetrogenetic Implications for Ophiolite Ultramafic Bodies from Lokris and Beotia (Central Greece) Based on Chemistry of Their Cr-spinels
JournalGeosciences
AuthorsPomonis, PanagiotisAuthor
Magganas, AndreasAuthor
Year2017 (March 3)Volume7
Page(s)10Issue1
PublisherMDPI AG
URL
Download URLhttps://www.mdpi.com/2076-3263/7/1/10/pdf?version=1488537485
DOIdoi:10.3390/geosciences7010010Search in ResearchGate
Mindat Ref. ID1039687Long-form Identifiermindat:1:5:1039687:6
GUID8fa1acf1-13bb-4f07-9845-ba2f3c78d425
Full ReferencePomonis, Panagiotis, Magganas, Andreas (2017) Petrogenetic Implications for Ophiolite Ultramafic Bodies from Lokris and Beotia (Central Greece) Based on Chemistry of Their Cr-spinels. Geosciences, 7 (1) 10 doi:10.3390/geosciences7010010
Plain TextPomonis, Panagiotis, Magganas, Andreas (2017) Petrogenetic Implications for Ophiolite Ultramafic Bodies from Lokris and Beotia (Central Greece) Based on Chemistry of Their Cr-spinels. Geosciences, 7 (1) 10 doi:10.3390/geosciences7010010
In(2017, March) Geosciences Vol. 7 (1) MDPI AG

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.

Zaccarini (2011) Geol. Acta Chromite and platinum group elements mineralization in the Santa Elena Ultramafic Nappe (Costa Rica): geodynamic implications 9
()
Serpentinized, Residual Mantle Peridotites from the M.A.R. Median Valley, ODP Hole 670A (21° 10′N, 45° 02′W): Primary Mineralogy and Geothermometryhttp://www-odp.tamu.edu/Publications/106109SR/VOLUME/CHAPTERS/sr106109_04.pdf
Petrological Studies of Peridotites from Diapiric Serpentinite Seamounts in the Izu–Mariana Fore-Arc, Leg 125http://www-odp.tamu.edu/publications/125_SR/VOLUME/CHAPTERS/sr125_27.pdf
Economou-Eliopoulos (1999) Chem. Erde On the geochemistry of chromitites from the Pindos ophiolite complex, Greece 59, 19
Hatzipanagiotou (2001) Braunschweiger geowiss Arb Origin and evolution of ultramafic rocks from the Koziakas ophiolite‚ continental Greece 24, 235
Bortolotti (2004) Ofioliti Comparison among the Albanian and Greek ophiolites: In search of constraints for the evolution of the Mesozoic Tethys Ocean 29, 19
Rassios (2000) Geol. S. Am. S. Constraints on the formation and emplacement age of western Greek ophiolites (Vourinos, Pindos, and Othris) inferred from deformation structures in peridotites , 473
Langmuir (1993) Petrological systematics of mid-ocean ridge basalts: Constraints on melt generation beneath ocean ridges , 183
Trace Element Geochemistry of Peridotites from the Izu-Bonin-Mariana forearc, Leg 125http://www-odp.tamu.edu/publications/125_SR/VOLUME/CHAPTERS/sr125_28.pdf
Bloomer (1983) Gabbroic and ultramafic rocks from the Mariana Trench: An island arc ophiolite , 294


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