Russia, Khabarovsk Territory, village Sarapulskoye. The first and second photo, top-down: quaternary clay, sand, loam; basalt weathering crust; pillow lava; the lowest rocks are basalts. They are in the third photo. Pyroxene-olivine, olivine basalts. Form a cover. Gray, with a violet hue, dark gray, porous, with a porphyry structure. Phenocrysts are represented by: labrador, olivine, augite, hyperstene. Size from 0.5-1 to 2-3 mm. Epidote and chlorite are formed on pyroxenes. Iddingsite develops on olivine. The pores are usually filled with calcite, zeolites, chlorite and epidote.
Russia, Khabarovsk Territory, village Sarapulskoye. Pillow Lava. Pyroxene-olivine, olivine basalts. Form a cover. The age of the rocks is 15 million years. Kizinskaya series. Miocene.
Russia, Magadan region, left side of the Duck river. Quartz-albite diorite porphyrite with quartz-albite veins. These are the famous Ducks dykes. Dyke №7. The dyke is a slab-like body with a capacity of 0.5 m in the East to 3.5 m in the West, accompanied by apophyses that run parallel to the sedimentary rocks (lower Jurassic siltstone). It is traced to a depth of 250 meters. Xenoliths are rare. Sometimes there are intersecting, until the disappearance of dykes.
Russia, Primorsky Krai, right bank of the Ussuri River. Granites biotite, medium-grained, leucocratic. Shmakovsky granite-leucogranite complex, second phase. Upper Paleozoic (ancient Permian).
Russia, Primorsky Krai, Gorny Klyuchi village, right bank of the Ussuri River. Granites biotite, medium-grained, leucocratic. Shmakovsky granite-leucogranite complex, second phase. Upper Paleozoic (ancient Permian).
