Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia
This is an article in the field of earth sciences. The copper resources in Ningxia are relatively poor, and 15 copper producing areas have been basically identified, of which 6 deposits have been explored, and the accumulative amount of copper metal has been identified as 29210.71 tons. There are tw...
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| Format: | Article |
| Language: | zho |
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Institute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological Sciences
2024-02-01
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| Series: | Kuangchan zonghe liyong |
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| Online Access: | http://www.kczhly.com/en/article/doi/10.3969/j.issn.1000-6532.2024.01.004 |
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| author | Maoxin LU Liange XIANG Hong WANG Donggang WANG Fenghua MA Tong LI |
| author_facet | Maoxin LU Liange XIANG Hong WANG Donggang WANG Fenghua MA Tong LI |
| author_sort | Maoxin LU |
| collection | DOAJ |
| description | This is an article in the field of earth sciences. The copper resources in Ningxia are relatively poor, and 15 copper producing areas have been basically identified, of which 6 deposits have been explored, and the accumulative amount of copper metal has been identified as 29210.71 tons. There are two types of copper deposits: epigenetic medium-low temperature hydrothermal deposit and placer deposit. The mineralization process is magmatism, sedimentation,ore-bearing fluid process (non-magmatic-non-metamorphic process). Copper deposits are mainly distributed in Weining Beishan area, Xiangshan area, South West Huashan area and the southern area of Liupan Mountain. The metallogenic ages are Caledonian, Varissian, Indosinian and Yanshanian, mainly Caledonian and Yanshanian. According to the study on the metallogenic geological law of the existing deposits, the magmatic hydrothermal type and continental sedimentary type are taken as the key prediction types. According to the material composition of the ore-forming series, five ore-forming series related to copper are determined, and the ore-forming genealogy of copper ore is summarized. The research on metallogenic regularity of copper ore is improved. It provides a theoretical basis for the potential evaluation and prediction of copper resources in Ningxia. |
| first_indexed | 2024-04-24T20:24:15Z |
| format | Article |
| id | doaj.art-dfdd4087643d4b29b31478b79603fae1 |
| institution | Directory Open Access Journal |
| issn | 1000-6532 |
| language | zho |
| last_indexed | 2024-04-24T20:24:15Z |
| publishDate | 2024-02-01 |
| publisher | Institute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological Sciences |
| record_format | Article |
| series | Kuangchan zonghe liyong |
| spelling | doaj.art-dfdd4087643d4b29b31478b79603fae12024-03-22T07:31:13ZzhoInstitute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological SciencesKuangchan zonghe liyong1000-65322024-02-01451273110.3969/j.issn.1000-6532.2024.01.0042024-01lumaoxinGeological Characteristics and Metallogenic Regularity of Copper Deposits in NingxiaMaoxin LU0Liange XIANG1Hong WANG2Donggang WANG3Fenghua MA4Tong LI5Ningxia Institute of Basic Geological Survey, Yinchuan 750000, Ningxia, ChinaNingxia Institute of Basic Geological Survey, Yinchuan 750000, Ningxia, ChinaNingxia Institute of Basic Geological Survey, Yinchuan 750000, Ningxia, ChinaNingxia Institute of Basic Geological Survey, Yinchuan 750000, Ningxia, ChinaNingxia Institute of Basic Geological Survey, Yinchuan 750000, Ningxia, ChinaNingxia Institute of Basic Geological Survey, Yinchuan 750000, Ningxia, ChinaThis is an article in the field of earth sciences. The copper resources in Ningxia are relatively poor, and 15 copper producing areas have been basically identified, of which 6 deposits have been explored, and the accumulative amount of copper metal has been identified as 29210.71 tons. There are two types of copper deposits: epigenetic medium-low temperature hydrothermal deposit and placer deposit. The mineralization process is magmatism, sedimentation,ore-bearing fluid process (non-magmatic-non-metamorphic process). Copper deposits are mainly distributed in Weining Beishan area, Xiangshan area, South West Huashan area and the southern area of Liupan Mountain. The metallogenic ages are Caledonian, Varissian, Indosinian and Yanshanian, mainly Caledonian and Yanshanian. According to the study on the metallogenic geological law of the existing deposits, the magmatic hydrothermal type and continental sedimentary type are taken as the key prediction types. According to the material composition of the ore-forming series, five ore-forming series related to copper are determined, and the ore-forming genealogy of copper ore is summarized. The research on metallogenic regularity of copper ore is improved. It provides a theoretical basis for the potential evaluation and prediction of copper resources in Ningxia.http://www.kczhly.com/en/article/doi/10.3969/j.issn.1000-6532.2024.01.004earth sciencescopper mineprediction typemetallogenic regularitymetallogenic seriesmetallogenic lineage |
| spellingShingle | Maoxin LU Liange XIANG Hong WANG Donggang WANG Fenghua MA Tong LI Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia Kuangchan zonghe liyong earth sciences copper mine prediction type metallogenic regularity metallogenic series metallogenic lineage |
| title | Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia |
| title_full | Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia |
| title_fullStr | Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia |
| title_full_unstemmed | Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia |
| title_short | Geological Characteristics and Metallogenic Regularity of Copper Deposits in Ningxia |
| title_sort | geological characteristics and metallogenic regularity of copper deposits in ningxia |
| topic | earth sciences copper mine prediction type metallogenic regularity metallogenic series metallogenic lineage |
| url | http://www.kczhly.com/en/article/doi/10.3969/j.issn.1000-6532.2024.01.004 |
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