Abstract
Late Mesozoic Aginskaya tectono-magmatic structure was formed in the lower part of brittle earths crust. It has no direct or indirect manifestation in the morphostructure of the region, being localized over TMA zone of NE strike as magmatic focus by the mantle activization. Its ring-shaped morphology and ore zonality were formed by magma differentiation. Its manifestation on space images as lineament pattern occurs due to springtime development of plant communities, which are indicators of small landforms.
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