The Lower Mantle Minerals in Ophiolite-hosted Diamond
Ophiolites are fragments of ancient ocean lithosphere emplaced on continental margins, in island arcs or in accretionary prisms, and have long been studied to better understand the evolution of ocean basins and collision of tectonic plates, the processes of mountain building and the occurrence of va...
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| Veröffentlicht in: | Acta geologica Sinica (Beijing) 2015-12, Vol.89 (s2), p.108-109 |
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| Hauptverfasser: | , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
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| Online-Zugang: | Volltext |
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| Zusammenfassung: | Ophiolites are fragments of ancient ocean lithosphere emplaced on continental margins, in island arcs or in accretionary prisms, and have long been studied to better understand the evolution of ocean basins and collision of tectonic plates, the processes of mountain building and the occurrence of valuable ore bodies, such as podiform chromitites （Dilek and Fumes, 2011）. |
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| ISSN: | 1000-9515 1755-6724 |
| DOI: | 10.1111/1755-6724.12308_65 |