Evidence of crystallization in residual, Cl–F-rich, agpaitic, trachyphonolitic magmas and primitive Mg-

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Evidence of crystallization in residual, Cl–F-rich, agpaitic, trachyphonolitic magmas and primitive Mg-

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journal_title：Geological Magazine
Contributor：LEONE MELLUSO ; ROBERTO DE' GENNARO ; LORENZO FEDELE ; LUIGI FRANCIOSI ; VINCENZO MORRA
Publisher：Cambridge University Press
Date：2012-
Format：text/html
Language：en
Identifier：10.1017/S0016756811001099
journal_abbrev：Geological Magazine
issn：0016-7568
volume：149
issue：3
firstpage：551
section：Corrigendum

摘要

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).