{"title":"Subsoil Natural Physico-Chemical Reactor: Regularity of Natural Processes of Synthesis of Perfect Diamond Crystals","authors":"J. Svoreň","doi":"10.17265/2328-2193/2020.04.005","DOIUrl":null,"url":null,"abstract":": Studies of inclusions (defects) in minerals have shown that the source of carbon in the natural processes of synthesis of perfect diamond crystals is mantle carbon dioxide, ( СО 2 ) Р = 6.1 М P а and δ 13 С = (-6.1±0.5)‰. A new mechanism for the synthesis of natural crystals of diamond, pyrope, magnetite, quartz, etc. has been developed. It is shown that under the influence of a powerful pulse of tectonogenic energy in some parts of the lithosphere that there are deep faults-tubes, which take root-migrating melt in the direction of the earth’s crust. During migration in the contact zone—“melt-lithosphere rocks” due to their contact interaction-friction, a high-voltage electric field of complex shape is formed, in which CO 2 turns into an energy-excited state, its molecules decompose into individual radicals and atoms. In the melt-electrolyte under the influence of an electric field, ions-cations move in certain directions depending on the configuration of the field, which is due to magma, contact with rocks of the lithosphere and the speed of magma in the gap-tube. As they move, these ions undergo numerous collisions with the molecules present there, in particular, СО 2 and its atoms and radicals, temporarily forming unstable compounds that fall into the zone with existing iron compounds, etc. Oxygen СО 2 poatomically detaches from the molecule and forms FeO · Fe 2 O 3 (magnetite), and the most energetically advantageous for chemically active carbon atoms in such an environment is that the melt bonds together form a diamond crystal. The isolated SiO 2 molecules chemically form a group of garnets, quartz, and the like.","PeriodicalId":66051,"journal":{"name":"地质资源与工程:英文版","volume":" ","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2020-08-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"地质资源与工程:英文版","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.17265/2328-2193/2020.04.005","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 2
Abstract
: Studies of inclusions (defects) in minerals have shown that the source of carbon in the natural processes of synthesis of perfect diamond crystals is mantle carbon dioxide, ( СО 2 ) Р = 6.1 М P а and δ 13 С = (-6.1±0.5)‰. A new mechanism for the synthesis of natural crystals of diamond, pyrope, magnetite, quartz, etc. has been developed. It is shown that under the influence of a powerful pulse of tectonogenic energy in some parts of the lithosphere that there are deep faults-tubes, which take root-migrating melt in the direction of the earth’s crust. During migration in the contact zone—“melt-lithosphere rocks” due to their contact interaction-friction, a high-voltage electric field of complex shape is formed, in which CO 2 turns into an energy-excited state, its molecules decompose into individual radicals and atoms. In the melt-electrolyte under the influence of an electric field, ions-cations move in certain directions depending on the configuration of the field, which is due to magma, contact with rocks of the lithosphere and the speed of magma in the gap-tube. As they move, these ions undergo numerous collisions with the molecules present there, in particular, СО 2 and its atoms and radicals, temporarily forming unstable compounds that fall into the zone with existing iron compounds, etc. Oxygen СО 2 poatomically detaches from the molecule and forms FeO · Fe 2 O 3 (magnetite), and the most energetically advantageous for chemically active carbon atoms in such an environment is that the melt bonds together form a diamond crystal. The isolated SiO 2 molecules chemically form a group of garnets, quartz, and the like.