Description of the conditions for differentiation of melts and solutions in the mantle and crust
Melt is a solution of electrolyte and its structure under РГ-conditions of the mantle is similar to the structure of water solution. As independent parameters describing its behavior under constant pressure and temperature we propose to use characteristics Eh and pH. Detailed reconstruction of physi...
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| Datum: | 2012 |
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| Format: | Artikel |
| Sprache: | Russisch |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2012
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| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/116668 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543275384569856 |
|---|---|
| author | Usenko, O. V. |
| author_facet | Usenko, O. V. |
| author_sort | Usenko, O. V. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T12:21:20Z |
| description | Melt is a solution of electrolyte and its structure under РГ-conditions of the mantle is similar to the structure of water solution. As independent parameters describing its behavior under constant pressure and temperature we propose to use characteristics Eh and pH. Detailed reconstruction of physical-chemical interactions taking place in the mantle and crust permits to solve not only theoretical problems but also essentially localize the sites of search of mineral deposits related to magmatic melts and hydrothermal solutions. |
| first_indexed | 2025-07-17T11:07:25Z |
| format | Article |
| id | journalsuranua-geofizicheskiy-article-116668 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:07:25Z |
| publishDate | 2012 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-1166682020-10-07T12:21:20Z Description of the conditions for differentiation of melts and solutions in the mantle and crust Usenko, O. V. Melt is a solution of electrolyte and its structure under РГ-conditions of the mantle is similar to the structure of water solution. As independent parameters describing its behavior under constant pressure and temperature we propose to use characteristics Eh and pH. Detailed reconstruction of physical-chemical interactions taking place in the mantle and crust permits to solve not only theoretical problems but also essentially localize the sites of search of mineral deposits related to magmatic melts and hydrothermal solutions. S. Subbotin Institute of Geophysics of the NAS of Ukraine 2012-10-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/116668 10.24028/gzh.0203-3100.v34i5.2012.116668 Geofizicheskiy Zhurnal; Vol. 34 No. 5 (2012); 116-131 Геофизический журнал; Том 34 № 5 (2012); 116-131 Геофізичний журнал; Том 34 № 5 (2012); 116-131 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/116668/110744 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| spellingShingle | Usenko, O. V. Description of the conditions for differentiation of melts and solutions in the mantle and crust |
| title | Description of the conditions for differentiation of melts and solutions in the mantle and crust |
| title_full | Description of the conditions for differentiation of melts and solutions in the mantle and crust |
| title_fullStr | Description of the conditions for differentiation of melts and solutions in the mantle and crust |
| title_full_unstemmed | Description of the conditions for differentiation of melts and solutions in the mantle and crust |
| title_short | Description of the conditions for differentiation of melts and solutions in the mantle and crust |
| title_sort | description of the conditions for differentiation of melts and solutions in the mantle and crust |
| url | https://journals.uran.ua/geofizicheskiy/article/view/116668 |
| work_keys_str_mv | AT usenkoov descriptionoftheconditionsfordifferentiationofmeltsandsolutionsinthemantleandcrust |