Occurs at the inner contact with lithium pegmatite around oligoclase andesite. Discredited as a mixture of two distinct amphibole compositions, tremolite and a new amphibole end-mem ber, Fluoro-sodic-pedrizite,
IMA Status:
Discredited IMA 2005
Locality:
Tastyg spodumene deposit, Tuva, Siberia, Russia, Link to MinDat.org Location Data.
Name Origin:
Named for its monoclinic crystal structure and relationship with holmsquisite. Approved IMA 1985, Discredited IMA 2005 as being fluoro-sodic-pedrizite.