Solar System Processes Underlying Planetary Formation, Geodynamics, and the Georeactor |
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| Authors: | J Marvin Herndon |
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| Institution: | (1) Transdyne Corporation, 11044 Red Rock Drive, San Diego, CA 92131, USA |
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| Abstract: | Only three processes, operant during the formation of the Solar System, are responsible for the diversity of matter in the
Solar System and are directly responsible for planetary internal-structures, including planetocentric nuclear fission reactors,
and for dynamical processes, including and especially, geodynamics. These processes are: (i) Low-pressure, low-temperature
condensation from solar matter in the remote reaches of the Solar System or in the interstellar medium; (ii) High-pressure,
high-temperature condensation from solar matter associated with planetary-formation by raining out from the interiors of giant-gaseous
protoplanets, and; (iii) Stripping of the primordial volatile components from the inner portion of the Solar System by super-intense
solar wind associated with T-Tauri phase mass-ejections, presumably during the thermonuclear ignition of the Sun. As described
herein, these processes lead logically, in a causally related manner, to a coherent vision of planetary formation with profound
implications including, but not limited to, (a) Earth formation as a giant gaseous Jupiter-like planet with vast amounts of
stored energy of protoplanetary compression in its rock-plus-alloy kernel; (b) Removal of approximately 300 Earth-masses of
primordial volatile gases from the Earth, which began Earth’s decompression process, making available the stored energy of
protoplanetary compression for driving geodynamic processes, which I have described by the new whole-Earth decompression dynamics
and which is responsible for emplacing heat at the mantle-crust-interface at the base of the crust through the process I have
described, called mantle decompression thermal-tsunami; and, (c) Uranium accumulations at the planetary centers capable of
self-sustained nuclear fission chain reactions. |
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| Keywords: | crustal heat Earth core Earth structure georeactor geodynamics geo-antineutrino Solar System formation thermal-tsunami whole-Earth decompression dynamics |
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