Abstract
57 Postmagmatic parageneses of the Eifel volcanic field (Germany) are characterized by a wide variety of minerals [1]. Gunterblassite 1 is a new mineral discov� ered in a late association formed in the cavities of the alkaline basalt of the Rother Kopf mountain. The chemical composition was determined by electron microprobe analysis. The content of H 2 O was quanti� fied by chromatographic analysis of gaseous products of calcination. The IR spectrum of the mineral shows the absence of borate, carbonate, nitrate, and ammo� nium groups. The empirical formula calculated for 13 atoms (Si, Al) is
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