Recognition and Mapping of Structural Guides for Barytes Mineral Exploration in Parts of Kadapa District using Remote Sensing and GIS

M. Ramachandra, K. Raghubabu, B. Kumar, P. S. Reddy
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引用次数: 2

Abstract

Identification and mapping of structural criteria of a region reveals information about the occurrence of ore deposits of igneous and metamorphic origin. Remote Sensing and GIS data helps in detection of such structural features, like faults, lineament, folds, etc. These are important guides for exploration of ore mineral and groundwater. Kadapa district hosts important ore minerals of igneous and metamorphic origin like Barytes, asbestos, gold, galena, steatite etc. Barytes is exploited in the district since a long past. Present study is taken up to prepare structural map along the existing Barytes mines in the district using geospatial techniques like Remote Sensing and GIS, with an intension to identify new Barytes mineralized locations through these structural guides. The structural data of any region provides a quick payback with faster, more accurate mineral identification for gold, silver, diamonds, iron, nickel, copper, uranium, aluminum, Barytes, and also provide rock and mineral relationship in search for ore deposits during exploration. Structural criteria, is an important measure in mineral exploration of certain mineral deposits that are confined by geographic, geological and tectonic features. Mainly the occurrence of ore deposits is dependent on neighboring lithology and structural deformation of the location area. Endogenous mineral deposits like tin, muscovite, lithium, tungsten, gold, beryl, gemstones etc. are associated with intermediate and acid rocks like syenite; granite, granodiorite. etc., and deposits of copper, nickel, cobalt, silver, arsenic and apatite are formed in basic rocks like gabbro, norite, diorite, etc. Due to false nature of ore bodies and their varied controls of mineralization the techniques used for mineral exploration such as remote sensing followed by ground and airborne geophysical surveys, stream sediment, litho-geochemical surveys and core drilling have been used for regional and detailed surveys. The aspect that indicate the mineralisation are known as localizers. If these indicators can be identified on satellite data/imagery then the mineral explorations can be much faster with increased efficiency. Keywords: Multispectral, LISS-III Satellite Imagery, SOI Toposheet remote sensing, GIS Cite this Article Ramachandra M., Raghu Babu K., Pradeep Kumar B. et al. Recognition and Mapping of Structural Guides for Barytes Mineral Exploration in Parts of Kadapa District using Remote Sensing and GIS. Journal of Remote Sensing & GIS . 2018; 9(3): 30–36p.
基于遥感和GIS的Kadapa地区部分重晶石找矿构造导图识别与成图
一个地区构造标准的识别和填图,揭示了火成岩和变质岩矿床的产状信息。遥感和地理信息系统数据有助于检测这些结构特征,如断层、地貌、褶皱等。这对矿产资源勘查和地下水勘查具有重要指导意义。卡达帕地区拥有重晶石、石棉、金、方铅矿、滑石等重要的火成岩和变质成矿矿物。这个地区很久以前就开始开采重晶石。目前的研究是利用遥感和地理信息系统等地理空间技术编制该地区现有重晶石矿山的结构图,目的是通过这些结构指南确定新的重晶石矿化位置。任何地区的构造数据都可以为金、银、钻石、铁、镍、铜、铀、铝、重晶石的更快、更准确的矿物识别提供快速回报,并在勘探过程中为寻找矿床提供岩石和矿物关系。构造标志是对某些受地理、地质和构造特征限制的矿床进行找矿的一项重要措施。矿床的产状主要取决于邻近的岩性和定位区的构造变形。内源性矿床,如锡、白云母、锂、钨、金、绿柱石、宝石等,与正长岩等中酸性岩石有关;花岗岩、花岗闪长岩。辉长岩、黑长岩、闪长岩等基性岩中形成铜、镍、钴、银、砷、磷灰石等矿床。由于矿体的虚假性质及其对矿化的不同控制,用于矿产勘探的技术,如遥感,然后是地面和航空地球物理测量,水系沉积物,岩石地球化学测量和岩心钻探,已用于区域和详细测量。指示矿化的面被称为定位面。如果可以根据卫星数据/图像确定这些指标,那么矿物勘探就可以更快,效率也会提高。关键词:多光谱,LISS-III卫星图像,SOI Toposheet遥感,GIS基于遥感和GIS的Kadapa地区部分重晶石找矿构造导图识别与成图遥感与地理信息系统学报。2018;9 (3): 30-36p。
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