Geology |
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| Pillow-like globules in the combined dykes. Zones of quenching are observed in basalt isolations (Usty Khilok massif). | Large (to 1 meter and more) basalt globules in 5 meter combined dyke of the Shaluty quartz syenite massif. | Trachybasalt lavas of the Tamir volcano-tectonic structure. |
