Petrology of Al- and Cr-rich ophiolitic chromitites from the Muğla, SW Turkey: implications from composition of chromite, solid inclusions of platinum-group mineral, silicate, and base-metal mineral, and Os-isotope geochemistry
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-009-0402-9.pdf
Reference53 articles.
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2. Alard O, Luguet A, Pearson NJ, Griffin WL, Lorand JP, Gannoun A, Burton KW, O’Reilly SY (2005) In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle. Nature 436:1005–1008. doi: 10.1038/nature03902
3. Alçiçek MC (2007) Tectonic development of an orogen-top rift recorded by its terrestrial sedimentation pattern: the Neogene Eşen Basin of southwestern Anatolia, Turkey. Sediment Geol 200:117–140. doi: 10.1016/j.sedgeo.2007.04.003
4. Arai S, Uesugi J, Ahmed AH (2004) Upper crustal podiform chromitite from the northern Oman ophiolite as the stratigraphically shallowest chromitite in ophiolite and its implication for Cr concentration. Contrib Mineral Petrol 147:145–154. doi: 10.1007/s00410-004-0552-8
5. Arai S, Kodoshima K, Morishita K (2006) Widespread arc-related melting in the mantle section of the northern Oman ophiolite as inferred from detrial chromian spinels. J Geol Soc 163:869–879. doi: 10.1144/0016-76492005-057
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