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The article discusses the composition, structure, and origin of carbonate concretions found in the South Kambalnyi Central Thermal Field in Kamchatka. These concretions, primarily composed of aragonite, contain various chemical compounds and exhibit diverse structures, indicating a complex formation process linked to hydrothermal activity. The study highlights their significance in understanding the geothermal system and the conditions of metalliferous solution discharge in the area.

Author

beenamol

Language

EN