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A HACONS.mantle fluid,has been proposed in the light of current knowledge concerning Diwa,rift,asthenosphere,anomalous and depleted mantle,plume,percolating magma fluid,degassing,inorganic origin of some oil and gas,hypogenic salt deposits,alkali-metasomatism in hydrothermal depos-its and experimental studies of basalts.The HACONS fluid originated from the mantle and is composed ofhydrogen and halogens (H).alkalis (A),carbon (C),oxygen (O),nitrogen (N) and sulfur (S) com-pound systems.Aluminosilicate magmas are expected when the HACONS fluid reacts with solid rocks.Many geological processes,including tectonism,magmatism,volcanism,metamorphism,hydrothermalactivity,thermal sedimentation and related mineralizations are thought to be controlled to a certain extentby large scale movement of HACONS fluid in the earth’s interior.The asthenosphere is essentially a layerwith abundant HACONS fluid.
A HACONS.mantle fluid, has been proposed in the light of current oil concerning Diwa, rift, asthenosphere, anomalous and depleted mantle, plume, percolating magma fluid, degassing, inorganic origin of some oil and gas, hypogenic salt deposits, alkali-metasomatism in hydrothermal depos-its and experimental studies of basalts. The HACONS fluid originated from the mantle and is composed of hydrogen and halogens (H). alkalis (A), carbon (C), oxygen (O) S) com-pound systems. Aluminum silicate magmas are expected when the HACONS fluid reacts with solid rocks.Many geological processes, including tectonism, magmatism, volcanism, metamorphism, hydrothermalactivity, thermal sedimentation and related mineralizations are thought to be controlled to a certain extentby large scale movement of HACONS fluid in the earth’s interior. The asthenosphere is essentially a layer with abundant HACONS fluid.