Abstract
Zeolites that fill vugs in basalt from the type locality of “doranite” near Carrickfergus, UK, were reexamined with the hope of establishing the magnesium analog of analcime as a valid species. However, contents 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 diffraction and optical microscopy show a vug assemblage of thomsonite + natrolite + analcime + Mg-rich clay minerals.
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