Mantle Ichor HACONS—Evidence of Its Existence（I）

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,hypogeic 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),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,hydrothermal activity,thermal sedimentation and related mineralizations are thought to be controlled to a certain extent by large -scale mouement of HACONS fluid in the earth‘s interior.The asthenosphere is essentially a layer with abundant HACONS fluid.

Mantle ichor HACONS — Evidence of its existence (I)

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 deposits 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), nitrogen (N) and sulfur (S) compound systems. Aluminosilicate magmas are expected when the HACONS fluid reacts with solid rocks. Many geological processes, including tectonism, magmatism, volcanism, metamorphism, hydrothermal activity, thermal sedimentation and related mineralizations are thought to be controlled to a certain extent by large scale movement of HACONS fluid in the earth’s interior. The asthenosphere is essentially a layer with abundant HACONS fluid.