Natural carbon nanofibers have been found in diamond-bearing carbonatites from the Chagatay trachyte-carbonatite complex (Uzbekistan) and described using a series of methods, including SEM, TEM, and Raman spectroscopy. The carbon nanofibers occur as tight aggregates within the host graphite, forming natural bulk nano-structural intergrowths. This is the first description of such carbon nanofibers either in nature or in the laboratory. The data from this study suggest a new possible means of diamond formation. These carbon intergrowths could potentially be used as a model for the fabrication of new types of carbon nanostructural material.
Evidence for extreme fractionation of peralkaline silicic magmas, the Boseti volcanic complex, main Ethiopian Rift / Macdonald, R., Baginski, B., Ronga, F., Dzierzanowski, P., Lustrino, M., Marzoli, A., Melluso, L.. - In: MINERALOGY AND PETROLOGY. - ISSN 0930-0708. - 104:(2012), pp. 163-175. [10.1007/s00710-011-0184-4]
Evidence for extreme fractionation of peralkaline silicic magmas, the Boseti volcanic complex, main Ethiopian Rift
MELLUSO, LEONE
2012
Abstract
Natural carbon nanofibers have been found in diamond-bearing carbonatites from the Chagatay trachyte-carbonatite complex (Uzbekistan) and described using a series of methods, including SEM, TEM, and Raman spectroscopy. The carbon nanofibers occur as tight aggregates within the host graphite, forming natural bulk nano-structural intergrowths. This is the first description of such carbon nanofibers either in nature or in the laboratory. The data from this study suggest a new possible means of diamond formation. These carbon intergrowths could potentially be used as a model for the fabrication of new types of carbon nanostructural material.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.


