作者: A.E Williams-Jones , S.A Wood
DOI: 10.1016/0016-7037(91)90042-4
关键词: Fluorite 、 Pluton 、 Carbonate minerals 、 Batholith 、 Fluid inclusions 、 Rare-earth element 、 Geochemistry 、 Mineralization (geology) 、 Geology 、 Igneous rock 、 Geochemistry and Petrology
摘要: This paper is in response to an earlier by R. Lira and E. M. Ripley. acknowledges the significant contribution previous authors made understanding of physiochemical conditions attending hydrothermal rare earth element (REE) mineralization. They conclude, however, that there a general lack information on deposition bastnaesite, which principal ore mineral most REE deposits. It their opinion behavior aqueous-carbonic fluid inclusions fluorite more complex than those reported former authors. are concerned actual temperature pressure formation for assemblage bastnaesite-fluorite-calcite may be significantly lower proposed.