Zeolites that fill vugs in basalt from the type locality of ''doranite
'' near Carrickfergus, UK, were reexamined with the hope of establishi
ng the magnesium analog of analcime as a valid species. However, conte
nts of Mg in the zeolites as measured by electron microprobe analysis
were not above the limits of detection (0.01 wt% MgO). X-ray powder di
ffraction and optical microscopy show a vug assemblage of thomsonite natrolite + analcime + Mg-rich clay minerals.