Application of ALI, ASTER and World View-2 imagery for mineral prospecting – a case study in the Maizijing-Shulonggou area, Ningxia Hui autonomous region, China
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摘要
To explore clues for gold prospecting in the Maizijing-Shulonggou area, Ningxia Hui autonomous region, China, this study extracted geological information related to fracture zones and hydrothermal alterations using ALI, ASTER, and World View-2 data, and subsequently, explored potential relationships between extracted geological characteristics and gold mineralization. The World View-2 image in the study area was used for fracture interpretation. The azimuth and density of linear fractures were investigated, and the results showed that linear fractures with NE direction were most common, identified gold mineralization spots except Au2 were all located in NE fracture zones, and all gold mineralization spots located in high fracture density areas where NE and NW fractures were the most common observations. Hydrothermal alteration minerals in exposed bedrocks were mapped using ALI and ASTER data. The spatial distribution of alteration minerals revealed regional specific alteration mineral in gold mineralization. In the northern Maizijing region, the composition of alteration mineral in the surrounding of Au1 was overwhelmed by quartz, while the alteration minerals in the surrounding of Au2-4 were dominated by limonite in the southern Shulonggou region. In the southern Shulonggou region, pyrite in buried quartz-pyritization belt and illitization-pyritization belt is likely to be the precursor of limonite. Heavy mineral assemblages were analyzed for native gold content, and the results suggested high native gold content in the illitization-pyritization belt, followed by quartz-pyritization belt, which was consistent with the strong association of limonite and gold mineralization.
To explore clues for gold prospecting in the Maizijing-Shulonggou area, Ningxia Hui autonomous region, China, this study extracted geological information related to fracture zones and hydrothermal alterations using ALI, ASTER, and World View-2 data, and subsequently, explored potential relationships between extracted geological characteristics and gold mineralization. The World View-2 image in the study area was used for fracture interpretation. The azimuth and density of linear fractures were investigated, and the results showed that linear fractures with NE direction were most common, identified gold mineralization spots except Au2 were all located in NE fracture zones, and all gold mineralization spots located in high fracture density areas where NE and NW fractures were the most common observations. Hydrothermal alteration minerals in exposed bedrocks were mapped using ALI and ASTER data. The spatial distribution of alteration minerals revealed regional specific alteration mineral in gold mineralization. In the northern Maizijing region, the composition of alteration mineral in the surrounding of Au1 was overwhelmed by quartz, while the alteration minerals in the surrounding of Au2-4 were dominated by limonite in the southern Shulonggou region. In the southern Shulonggou region, pyrite in buried quartz-pyritization belt and illitization-pyritization belt is likely to be the precursor of limonite. Heavy mineral assemblages were analyzed for native gold content, and the results suggested high native gold content in the illitization-pyritization belt, followed by quartz-pyritization belt, which was consistent with the strong association of limonite and gold mineralization.
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