Modification of the High-Pressure-Type Chromites into the Low- Pressure-Type： Petrological Investigation of the Podiform Chromitites in the Luobusa Ophiolite, Tibet
The podiform chromitites in the Luobusa ophiolite, Southem Tibet, have received much attention because of the presence of ultrahigh-pressure minerals, such as micro- diamonds （Bai et al., 1993; Yang et al., 2007; Xu et al.,
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| Veröffentlicht in: | Acta geologica Sinica (Beijing) 2015-12, Vol.89 (s2), p.104-104 |
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| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
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| Online-Zugang: | Volltext |
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| Zusammenfassung: | The podiform chromitites in the Luobusa ophiolite, Southem Tibet, have received much attention because of the presence of ultrahigh-pressure minerals, such as micro- diamonds （Bai et al., 1993; Yang et al., 2007; Xu et al., |
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| ISSN: | 1000-9515 1755-6724 |
| DOI: | 10.1111/1755-6724.12308_62 |