Le Maitre et al., (2005).
Kalsilite-bearing plutonic rocks are extremely rare. They have been described in the Palaeozoic to Mesozoic ultrapotassic massifs of the Baikal-Stanovoi Rift, Siberia (Synnyr, Sakun, Murun, and Yaksha), in the small Rischorr complex of the giant and predominantly sodic Devonian Khibiny Massif, and in the Ordovician ultramafic Batbjerg intrusion of East Greenland.
The largest Kalsilite-bearing plutons are confined to Baikal-Stanovoy rifting system and situated between metamorphic rocks of Pre-Cambrian and Early Cambrian ages. The Siberian massifs are epizonal, rhythmically layered massifs characterized by ultramafic and mafic rocks and often associated with carbonatites. In these massifs the synnyrites represent a small fraction of the massif volume, and are restricted to the upper layered series. Melano- and mesocratic rocks (mica pyroxenites, shonkinites, pulaskites) prevail within the lower series and the leucocratic ones (nepheline and pseudoleucite syenites, synnyrites) predominate within the upper series.
Fig.1: Structure of the Synnyr pluton with AB and CD geological sections. Modified from Zhidkov (1978).
) is an oval-shaped body with 3D funnel like morphology, intruding into a sedimentary sequence of Cambrian limestone, conglomerate and sandstone and Palaeozoic granitoids. From core to the rim following succession of rocks occur in following order: alkaline syenite, pseudoleucite syenite, microcline pseudoleucite syenite and nepheline syenite. At the central part the oval-shaped stock (100 km
), is an igneous complex comprising trachyte and pyroxene-syenite (pulaskite). One of the varieties of pseudoleucite-bearing rocks is synnyrite, consisting of microcline and intergrowth of orthoclase, kalsilite and sometime nepheline. In the intergrowth, the ratio of K-feldspar to kalsilite (+/- nepheline) varies between 67 and 33 vol%. The K
O content of these rocks may be as high as 18-20 wt%. The vol% of pseudoleucite may be as high as 50-60 %. During the final stage, dykes of tinguaite, shonkinite, camptonite and monchiquite were emplaced. Geological age dating determined through the Rb-Sr isotopic method from minerals of nepheline syenites yielded an age of 330 Ma.
• Panina, L., Sharygin, V., Proshenkin, I (1995): Synnyrites-New Complex Alumina-Potassic Raw Material. Shigen-Chishitsu, 45(252), 223-233.
Photo
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 2x (Field of view = 7mm) |
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 2x (Field of view = 7mm) |
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 2x (Field of view = 7mm) |
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 10x (Field of view = 2mm) |
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 10x (Field of view = 2mm) |
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. PPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 2x (Field of view = 7mm) |
Garnet (brown), pyroxene (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 2x (Field of view = 7mm) |
Garnet (brown), biotite (green) and feldspar (colorless). Synnyrite from Synnyr pluton. PPL image, 2x (Field of view = 7mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. PPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 10x (Field of view = 2mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |
K-feldspar-kalsilite intergrowth. Synnyrite from Synnyr pluton. XPL image, 20x (Field of view = 1mm) |