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Introduction
One of the central arguments in favor of the Big Bang theory is that it explains well the chemical abundance within the Cosmos. It describes, for example, why hydrogen and helium should vastly dominate the other elements as a percentage of visible matter and, in fact, this is precisely what is observed by astronomers. Thus, hydrogen and helium make up perhaps ninety-nine percent of the ordinary visible matter in the Universe. The elements heavier than hydrogen and helium up to iron are fused supposedly in the stars as they evolve by consuming their atomic components in fusion processes. Elements heavier than iron are catastrophically fused via supernovae explosions, the terminal phase of a stars fusion cycle. This is the orthodox convention.
For those scientists who disagree fundamentally with the Big Bang occurrence, their alternative theories have had difficulty explaining the dominance of hydrogen in the Universe. Thus a key question arises: If there was no Big Bang in the distant past, how can there be so much hydrogen as observed in the Cosmos? It is the approach of this paper that neutrino oscillations may provide such a plausible alternative mechanism whereby hydrogen can be fabricated without invoking a Big Bang-type creation event.
The other possibility is that if there was a Big Bang event, vastly less hydrogen was fabricated by it. Perhaps, neutrinos which were likely to be high energy in the early Universe, "off-loaded" their energy into the early planetary-type objects fabricating hydrogen atoms. Hence, hydrogen is created in the cores of the planets causing the evolution of such objects to larger bodies. This is an ongoing process today.
Moreover, the fusion of slow neutrons which then beta decay to fabricate higher elements may take place at or near the core of a planet. Thus, the fusion of hydrogen is taking place within planets as well as stars. The common beta-decay process, provides a standard mechanism which enables nuclide to nucleus fusion at low energies and provides a fabrication pathway to heavier elements over time. Another consideration is that hydrogen is joining-up with other elements to form simple molecules such as ordinary water and hydrated minerals in the liquid outer core. This offers a different explanation of the origin of the oceans on Earth.