The engineering and geological substantiation of the resource potential of the bed of the South China Sea

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 o...

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Bibliographic Details
Main Authors: Kirichenko, Y.V (Author), Ngo, T.T.Q (Author), Shchyokina, M.V (Author)
Format: Article
Language:English
Published: National University of Science and Technology MISIS 2023
Subjects:
Online Access:View Fulltext in Publisher
LEADER 03647nam a2200541Ia 4500
001 10.17073-2500-0632-2022-09-14
008 230526s2023 CNT 000 0 und d
020 |a 25000632 (ISSN) 
245 1 0 |a The engineering and geological substantiation of the resource potential of the bed of the South China Sea 
260 0 |b National University of Science and Technology MISIS  |c 2023 
300 |a 8 
856 |z View Fulltext in Publisher  |u https://doi.org/10.17073/2500-0632-2022-09-14 
520 3 |a 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 km2and 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. © Kirichenko Yu. V., Ngo T. T. Q., Shchyokina M. V., 2023. 
650 0 4 |a Crust 
650 0 4 |a crusts 
650 0 4 |a deep water areas 
650 0 4 |a Deep-water area 
650 0 4 |a deposit 
650 0 4 |a Deposits 
650 0 4 |a Economic geology 
650 0 4 |a Ferroalloys 
650 0 4 |a Ferromanganese formation 
650 0 4 |a ferromanganese formations 
650 0 4 |a Iron ores 
650 0 4 |a Mineral exploration 
650 0 4 |a Mining 
650 0 4 |a multiple factor analysis 
650 0 4 |a Multiple factor analysis 
650 0 4 |a Nodule 
650 0 4 |a nodules 
650 0 4 |a placers 
650 0 4 |a Placers 
650 0 4 |a Predictive prospect 
650 0 4 |a predictive prospects 
650 0 4 |a resource potential 
650 0 4 |a Resource potentials 
650 0 4 |a shelf 
650 0 4 |a Shelf 
650 0 4 |a South China sea 
650 0 4 |a South China Sea 
650 0 4 |a Viet Nam 
650 0 4 |a Vietnam 
650 0 4 |a zoning 
650 0 4 |a Zoning 
700 1 0 |a Kirichenko, Y.V.  |e author 
700 1 0 |a Ngo, T.T.Q.  |e author 
700 1 0 |a Shchyokina, M.V.  |e author 
773 |t Mining Science and Technology (Russian Federation)  |x 25000632 (ISSN)  |g 8 1, 5-12