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Evidence of crystallization in residual, Cl–F-rich, agpaitic, trachyphonolitic magmas and primitive Mg-rich basalt–trachyphonolite interaction in the lava domes of the Phlegrean Fields (Italy) – CORRIGENDUM

Published online by Cambridge University Press:  31 January 2012

LEONE MELLUSO ,
ROBERTO DE' GENNARO ,
LORENZO FEDELE ,
LUIGI FRANCIOSI  and
VINCENZO MORRA
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Extract

In an Original Article by Melluso et al. recently published online (1 November 2011), the mineral named as rosenbuschite should be named låvenite throughout, having the chemical composition broadly corresponding to the chemical formula (Na, Ca)2(Mn, Fe)(Zr, Ti)Si2O7(O, OH, F)2 (see Sørensen, 1997).

Information

Type
Corrigendum
Information
Geological Magazine , Volume 149 , Issue 3 , May 2012 , pp. 551
Copyright
Copyright © Cambridge University Press 2012

In an Original Article by Melluso et al. recently published online (1 November Reference Melluso, De' Gennaro, Fedele, Franciosi and Morra2011), the mineral named as rosenbuschite should be named låvenite throughout, having the chemical composition broadly corresponding to the chemical formula (Na, Ca)2(Mn, Fe)(Zr, Ti)Si2O7(O, OH, F)2 (see Sørensen, Reference Sørensen1997).

References

Melluso, L., De' Gennaro, R., Fedele, L., Franciosi, L. & Morra, V. Evidence of crystallization in residual, Cl–F-rich, agpaitic, trachyphonolitic magmas and primitive Mg-rich basalt–trachyphonolite interaction in the lava domes of the Phlegrean Fields (Italy). Geological Magazine, published online 1 November 2011. doi:10.1017/S0016756811000902.Google Scholar
Sørensen, H. 1997. The agpaitic rocks; an overview. Mineralogical Magazine 61, 485–98.CrossRefGoogle Scholar