Origin of Chromitites in the Songshugou Peridotite Massif, Qinling Orogen (Central China): Mineralogical and Geochemical Evidence
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/content/pdf/10.1007/s12583-019-1227-8.pdf
Reference86 articles.
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2. Arai, S., Matsukage, K., 1998. Petrology of a Chromitite Micropod from Hess Deep, Equatorial Pacific: A Comparison between Abyssal and Alpine-Type Podiform Chromitites. Lithos, 43(1): 1–14. https://doi.org/10.1016/s0024-4937(98)00003-6
3. Ballhaus, C., Wirth, R., Fonseca, R. O. C., et al., 2017. Ultra-High Pressure and Ultra-Reduced Minerals in Ophiolites may Form by Lightning Strikes. Geochemical Perspectives Letters, 5: 42–46. https://doi.org/10.7185/geochemlet.1744
4. Barnes, S. J., 2000. Chromite in Komatiites, II. Modification during Green-schist to Mid-Amphibolite Facies Metamorphism. Journal of Petrology, 41(3): 387–409. https://doi.org/10.1093/petrology/41.3.387
5. Barnes, S. J., Roeder, P. L., 2001. The Range of Spinel Compositions in Terrestrial Mafic and Ultramafic Rocks. Journal of Petrology, 42(12): 2279–2302. https://doi.org/10.1093/petrology/42.12.2279
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