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<article article-type="research-article" dtd-version="1.3" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">gscience</journal-id><journal-title-group><journal-title xml:lang="en">Mining Science and Technology (Russia)</journal-title><trans-title-group xml:lang="ru"><trans-title>Горные науки и технологии</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2500-0632</issn><publisher><publisher-name>The National University of Science and Technology MISiIS (NUST MISIS)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.17073/2500-0632-2022-09-14</article-id><article-id custom-type="elpub" pub-id-type="custom">gscience-415</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>MINERAL RESOURCES EXPLOITATION</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>РАЗРАБОТКА МЕСТОРОЖДЕНИЙ ПОЛЕЗНЫХ ИСКОПАЕМЫХ</subject></subj-group></article-categories><title-group><article-title>The Engineering and geological substantiation of the resource potential of the bed of the South China</article-title><trans-title-group xml:lang="ru"><trans-title>Инженерно-геологическое обоснование ресурсного потенциала дна Южно-Китайского моря</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кириченко</surname><given-names>Ю. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kirichenko</surname><given-names>Yu. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Юрий Васильевич Кириченко – доктор технических наук, профессор кафедры геологии и маркшейдерского дела.</p><p>Москва; Scopus ID 7007186248</p></bio><bio xml:lang="en"><p>Yuriy V. Kirichenko – Dr. Sci. (Eng.), Professor of the Department of Geology and Mine Surveying.</p><p>Moscow; Scopus ID 7007186248</p></bio><email xlink:type="simple">kirichenko.iv@misis.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Нго</surname><given-names>Ч. Т. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Ngo</surname><given-names>T. T. Q.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Чан Тхиен Кюи Нго – аспирант, Университет естественных наук.</p><p>Хошимин; Scopus ID 57222072264</p></bio><bio xml:lang="en"><p>Tran Thien Quy Ngo – PhD-Student, University of Science</p><p>Ho Chi Minh City, Scopus ID 57222072264</p></bio><email xlink:type="simple">nttquy@hcmus.edu.vn</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Щёкина</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Shchyokina</surname><given-names>M. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Марина Владимировна Щёкина – кандидат технических наук, доцент кафедры геологии и маркшейдерского дела.</p><p>Москва; Scopus ID 57271022000</p></bio><bio xml:lang="en"><p>Marina V. Shchyokina – Cand. Sci. (Eng.), Associate Professor of the Department of Geology and Mine Surveying.</p><p>Moscow; Scopus ID 57271022000</p></bio><email xlink:type="simple">mshchekina@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Университет науки и технологий МИСИС<country>Россия</country></aff><aff xml:lang="en">University of Science and Technology MISIS<country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru">Вьетнамский национальный университет Хошимина, Университет естественных наук<country>Вьетнам</country></aff><aff xml:lang="en">Viet Nam National University Ho Chi Minh City, University of Science<country>Viet Nam</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>20</day><month>04</month><year>2023</year></pub-date><volume>8</volume><issue>1</issue><fpage>5</fpage><lpage>12</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Kirichenko Y.V., Ngo T., Shchyokina M.V., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Кириченко Ю.В., Нго Ч., Щёкина М.В.</copyright-holder><copyright-holder xml:lang="en">Kirichenko Y.V., Ngo T., Shchyokina M.V.</copyright-holder><license license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://mst.misis.ru/jour/article/view/415">https://mst.misis.ru/jour/article/view/415</self-uri><abstract><p>The program for the development of the national economy based on own mineral raw materials as adopted in the Socialist Republic of Vietnam requires an increase the volumes of minerals. This includes both liquid hydrocarbons, and non-traditional solid minerals. This paper examines the resource base of mineral deposits in the South China Sea. The objective was to determine and scientifically establish classification criteria for zoning (regionalization), as well as to identify prospective areas with deposits of ferromanganese formations and other solid minerals. An analysis was undertaken of placers on the shelf and deposits of ferromanganese formations in the deep areas of the Vietnam Sea. A multiparameter analysis of the hydrological, geophysical, engineering and geological, environmental conditions of the deposit positions was conducted. In addition, criteria for the prospects of the formation and development of deposits of ferromanganese formations were established. These criteria enabled areas with different prospectivity ratings to be identified. Within the South China Sea, zones (areas) with a high, medium, and low potential for the presence of nodules were identified. Similar zoning for the crusts was also identified. The areas of these zones were determined. The results of the research established that the total potential area of ferromanganese nodules is 91,480 km2. The area with the potential of ferromanganese crusts is 2,421.6 km2, while the area of coexistence of nodules and crusts is 18,777 km2. Furthermore, priority regions for future exploration are those with high nodule potential covering an area of 18,110 km2 and the regions of high crust potential with an area of 882.6 km2. Based on the materials obtained, the bed of the Vietnamese Exclusive Zone of the South China Sea was zoned. Maps of the resource and predictive prospects of the seabed were drawn, and the prospecting and exploration operations can be established within this framework.</p></abstract><trans-abstract xml:lang="ru"><p>Принятая в Социалистической Республике Вьетнам программа развития народного хозяйства, базирующегося на собственной минерально-сырьевой базе, требует повышения объемов добычи полезных ископаемых, в том числе жидких углеводородов, вовлечения нетрадиционных видов твердых полезных ископаемых. Исследована ресурсная база месторождений полезных ископаемых Южно-Китайского моря. Идея исследований заключалась в определении и научном обосновании классификационных критериев зонирования (районирования) и выделении перспективных участков с залежами железомарганцевых образований и других твердых полезных ископаемых. Проведен анализ россыпных месторождений на шельфе и залежей железомарганцевых образований в глубинных районах Вьетнамского моря. Проведен многосторонний анализ гидрологических, геофизических, инженерно-геологических, экологических условий залегания месторождений, определены критерии перспективности образования и развития залежей железомарганцевых образований. Эти критерии позволили произвести выделение участков с различным рейтингом перспективности. В пределах Южно-Китайского моря выделены зоны (участки) с высоким, средним и низким потенциалом нахождения конкреций, а также выявлена аналогичная зональность для корок. Определены площади указанных зон. Результаты исследований показали, что общая потенциальная площадь железомарганцевых конкреций составляет 91 480 км2, площадь с потенциалом железомарганцевых корок – 2421,6 км2 и площадь сосуществования конкреций и корок – 18 777 км2. При этом приоритетными районами для будущих разведок являются районы с высоким потенциалом конкреций площадью 18 110 км2 и районы с высоким потенциалом корок площадью 882,6 км2. На основании полученных материалов произведено районирование дна Вьетнамской эксклюзивной зоны Южно-Китайского моря и составлены карты ресурсно-прогнозной перспективности морского дна, в пределах которых необходимо организовывать поисково-разведочные работы.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>ресурсный потенциал</kwd><kwd>шельф</kwd><kwd>глубоководные районы</kwd><kwd>многофакторный анализ</kwd><kwd>россыпи</kwd><kwd>железомарганцевые образования</kwd><kwd>месторождение</kwd><kwd>конкреции</kwd><kwd>корки</kwd><kwd>прогнозная перспективность</kwd><kwd>районирование</kwd><kwd>Южно-Китайское море</kwd><kwd>Вьетнам</kwd></kwd-group><kwd-group xml:lang="en"><kwd>resource potential</kwd><kwd>shelf</kwd><kwd>deep water areas</kwd><kwd>multiple factor analysis</kwd><kwd>placers</kwd><kwd>ferromanganese formations</kwd><kwd>deposit</kwd><kwd>nodules</kwd><kwd>crusts</kwd><kwd>predictive prospects</kwd><kwd>zoning</kwd><kwd>South China Sea</kwd><kwd>Vietnam</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Нго Чан Тхиен Кюи, Кириченко Ю.В., Щёкина М. 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