首页> 外文期刊>Research Journal of Applied Sciences: RJAS >Using SWIR Bands from ASTER for Discrimination of Hydrothermal Altered Minerals in the Northwest of Iran (Se-Sanandaj City); A Key for Exploration of Copper and Gold Mineralization
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Using SWIR Bands from ASTER for Discrimination of Hydrothermal Altered Minerals in the Northwest of Iran (Se-Sanandaj City); A Key for Exploration of Copper and Gold Mineralization

机译:利用ASTER的SWIR波段判别伊朗西北部(Se-Sanandaj市)的热液蚀变矿物;勘探铜金矿的关键

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We used SWIR bands from ASTER sensor data for mineral explorations in the west of Iran in Kurdistan Province in the southeast of Sanandaj city. The wavelength of SWIR bands is situated between 1.6-2.43 ?m. In these range, hydroxides minerals which have been produced by hydrothermal alteration have a good absorption compared to lower or upper wavelengths. Based on PCA and Band Ratios (BR) methods and so comparing reflectance-wavelength curves with NASA/JPL standard curves, we distinguished two Propylitic and Phyllic alteration zones; in Propylitic zone is rich in chlorite and epidote minerals and Phyllic zone is rich in white mica and kaolinite minerals. These 2 alteration zones are important for copper and gold mineralization in this part of Iran. In the last decade some gold mineralizations such as Kervian and Dashkasan have been explorated in the northwest and northeast of study area respectively.
机译:我们将来自ASTER传感器数据的SWIR波段用于Sanandaj市东南部库尔德斯坦省伊朗西部的矿物勘探。 SWIR波段的波长在1.6-2.43?m之间。在这些范围内,与较低或较高波长相比,通过水热改变产生的氢氧化物矿物具有良好的吸收。基于PCA和能带比(BR)方法,因此将反射率-波长曲线与NASA / JPL标准曲线进行比较,我们区分了两个原生质和质变区。在早产地带富含绿泥石和附子矿物,而Phyllic地带富含白云母和高岭石矿物。这两个蚀变带对伊朗这一地区的铜和金矿化非常重要。在过去的十年中,分别在研究区的西北部和东北部勘探了一些金矿,例如Kervian和Dashkasan。

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