Russian Mineralogical Society
200th Anniversary Meeting of the Russian Mineralogical Society
Genesis of eudialyte in the Lovozero alkaline massif

RMS-DPI code:  2017-1-264-0
Scientific session:  6. Mineral diversity and evolution of mineral formation processes.
Author listing:  Mikhailova J.A., Ivanjuk G.Y., Kalashnikov A.O., Yakovenchuk V.N., Pakhomovsky Ya.A., Bazai A.V.
Principal author:  Mikhailova Julia Alexandrovna
Language:  Russian
Abstract - Summary 
(short description):
The Lovozero alkaline comprises regularly alternating subhorizontal layers of low-Ca foyaite-malignite-shonkinite (“lujavrite”) and melteigite-urtite. Within these strata, there are numerous layer-like xenolites of basalt and basaltic tuff that transform under influence of alkaline melt into anorthoclase-dominant metasomatites enriched in diopside, richterite, titanite and (mangano)eudialyte. Both apo-basalt metasomatite and host “lujavrite” contain rich impregnation of (mangano)eudialyte grains with relics of parakeldyshite (commonly) or dalyite (rarely), which permits us to connect rich eudialyte mineralization with alteration of primary water-free zirconosilicates by Ca-rich fluid originated from the basalt fenitization.

Lovozero eudialyte complex, eudialyte malignite, basalt, alkaline metasomatite, parakeldyshite, eudialyte
 
RMS-DPI code:  2017-1-264-0
Pages:  268-270
File of proceedings 
(PDF): 
 191 K
Status:  printed
Accepted:  17/09/2017
Published on-line:  07/12/2017
Permanent address of publication:  http://www.minsoc.ru/2017-1-264-0/
Contact author(s):  Mikhailova, Julia Alexandrovna

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printed on 20/11/2019