Creation of Fe Isotopes in Natural Geology Crusts as the Result of Self-controlled Global Biostimulated LENR in Oceans and Seasстатья
Информация о цитировании статьи получена из
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 20 января 2021 г.
Аннотация:The paper considers the mechanism of formation of natural iron–manganese crusts, which are located at the bottom of all seas and oceans. These crusts are characterized by a periodic structure and an anomalous ratio of iron isotopes. These anomalies are similar in all seas and oceans and consist in excess of Fe54 and Fe56 isotope concentration and, accordingly, decrease of Fe57 isotope concentration compared to their standard values. It is shown that these anomalies are completely explained by the process of LENR (nuclear transmutation) in the bottom region of the seas and oceans, leading to nuclear fusion with the participation of manganese, sodium, and phosphorus and stimulated by the processes of natural metabolism of microbiological communities.