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
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
