Hydrothermal zonality of the Earth
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- Leningrad Mining Institute
Abstract
Water is the main driving force of inorganic life on the Earth. The state, structure, properties and composition of water depend on its temperature. The temperature of surface and underground natural waters of the Earth varies within very large limits and is subject to latitudinal climatic, altitudinal orographic and depth zonality. Hence the extreme diversity of natural waters and their interaction with the Earth's shells.
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