stripes
This occurrence consists of two bodies of nepheline and liebenerite syenite that cut through coarse- and medium-grained muscovitized syenites which grade into biotite syenites at depth – as indicated by drilling. The nepheline syenite bodies do not exceed 10 x 5 m and are composed mainly of alkali feldspar (40-50%), albite (5-20%), nepheline (2-50%), biotite (5-15%) and aegirine (5-20%). Accessory minerals are represented by titanite, zircon and apatite; overall they do not exceed 1-2%. The nepheline syenites vary from fine- to coarse-grained with pegmatitic varieties. The texture of the rocks may be gneiss-like or massive.
KUZNETSOVA, F.V. 1975. Nepheline syenites of the margin of the Borgoi depression. Nauka, Siberian Branch of the USSR Academy of Sciences, Novosibirsk. 92 pp.
PANINA, L.I. 1972. Mineral-genetic characteristic features of some alkaline massifs of the Baikal area. Nauka, Siberian Branch of the USSR Academy of Sciences, Novosibirsk, 127 pp.