共查询到18条相似文献,搜索用时 109 毫秒
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中等程度植被覆盖区岩石蚀变信息提取技术及其应用 总被引:4,自引:0,他引:4
各种类型的热液型矿产经常与围岩蚀变相伴生,蚀变岩类是找矿标志之一。陆地卫星TM数据在短波近红外范围内有二个波段,这两个波段的信息可用来进行蚀变岩的制图。可是在有部分或中等密度的植被复盖区,由于植被和蚀变岩类的反射光谱特性比较相似,影响了TM数据的制图能力。笔者开发了三种用来在中等程度植被复盖区进行蚀变岩类信息提取方法。这三种方法是:直接主成分分析法、最小平方拟合法和混合单元分解法。在滇黔桂微细浸染型金矿勘查中,这三种方法被成功地用来提取与金矿化有关的粘土蚀变岩类信息和制图。 相似文献
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利用TM数据快速提取含矿蚀变带方法研究 总被引:47,自引:5,他引:47
热液蚀变岩类是在含矿热液作用下引起原岩化学成分和物理性质发生变化的结果,因此蚀变岩类往往与内生产矿产伴生,有时其本身就是含矿体。不同蚀变矿特级组合具有独特的光谱响应,但是光谱的反射和吸收产特征较弱称为遥感找矿弱信息标志。 相似文献
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基于知识的蚀变遥感异常信息快速提取及找矿应用实践 总被引:1,自引:1,他引:1
本文以新疆卡拉先格尔成矿带内新发现的哈腊苏铜矿化区为例,进行ETM 矿化蚀变遥感异常信息快速提取研究.分别在ETM 1,ETM 2,ETM 3,ETM 4,ETM 5和ETM 7等6个波段图像和增强图像(比值图像、主成分分析图像)上已知蚀变岩分布区及地质背景进行像元光谱采样,并分析蚀变岩在ETM 的6个波段图像及铁染异常和羟基异常图像上的光谱特征,进而发现蚀变岩与矿区地层区分的光谱知识.利用矿区成矿地质特征和典型矿床成矿模型建立遥感地质找矿模型,发现遥感地质控矿特征.在此基础上建立了基于知识规则的在ETM 图像上提取蚀变遥感异常信息模型,利用ERDAS IMAGING V8.7图像处理系统中的专家分类器模块快速提取该区蚀变遥感异常信息,实现了地质与遥感在图像处理平台上的有机结合.经实际验证,其结果与实际情况基本吻合,并且新发现铜矿化带一处,可为与该区地质背景类似的新疆阿勒泰南缘开展铜矿普查勘探提供参考依据. 相似文献
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以西藏冈底斯成矿带中段江拉昂宗矽卡岩型铜多金属矿床作为研究区,基于ASTER遥感数据的多波段优势,应用比值法,对该矿区进行大理岩化、绿帘石化和透辉石化矿化信息的蚀变提取。在此基础上,建立蚀变对于成矿影响程度的判断,提高了遥感矿化蚀变信息识别精度。此方法应用性强,充分体现了此矿区及其外围蚀变规律,为江拉昂宗外围找矿提供了可靠依据。 相似文献
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基岩裸露区蚀变岩遥感信息的提取方法 总被引:43,自引:7,他引:36
笔者利用与金属矿化相关的蚀变岩的TM多波段图像像元亮度值曲线的双峰特性(TM3和TM5为高值),以柳沟峡地区为样区,进行了提取蚀变岩遥感信息的方法研究,改进了Crosta信息提取方法,认为用TM1+TM2、TM4/TM3、TM5、TM7组合进行主分量分析所获得的蚀变岩遥感异常图效果最佳。将该方法用于北祁连山西段,疏勒河以东9000km2区域内蚀变岩遥感信息提取,其结果是:在103处已知矿产地中的86处有蚀变岩遥感异常信息显示,符合率达83.5%,进而预测了找矿靶区115处。 相似文献
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矿物光谱指数是利用比值的方法增强Fe和含OH矿物在可见光、短波红外区间的吸收特征,进而提取蚀变矿物信息的一种方法。由于斑岩型矿床的蚀变分带特征明显,西藏多龙矿集区中集中了斑岩型、浅成低温热液型等铜、金矿床,通过矿物光谱指数的计算提取相关蚀变信息,对该区域的下一步找矿具有指导意义。本文采用矿物光谱指数(5+7)/6、(6+9)/8等方法提取了镁、铝两类羟基及铝羟基类下的高岭石等蚀变信息,采用5/4、2/1的方法提取了二价铁、三价铁的蚀变信息。经过与OLI影像采用PCA方法及野外实地勘查采样,证实了利用本文方法所提取的蚀变信息有效。 相似文献
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在太行山北段,王安镇、司各庄两个花岗杂岩体与区域成矿的关系密切。该区的成岩成矿受NNE、NE、SN、EW、NW走向构造带和环状构造的控制非常明显。其中SN与NW走向构造带与成矿关系最密切。构造主要控制岩体的侵位与展布方向和控制王安镇和司各庄岩体部分边界和几何形态。构造不仅可成为容矿构造,而且还控制蚀变岩石的分布。 相似文献
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Kaveh Pazand Jamal Fereidoni Sarvestani M. Reza S. Ravasan 《Journal of the Indian Society of Remote Sensing》2013,41(2):379-389
The Ahar area is located in East Azarbaijan province, and covers an area of about 2,500 km2. Spectral mapping techniques were applied on VNIR and SWIR of ASTER data for discriminating between hydrothermal alteration zones and the identification of high potential mineralized lithological unit associated with hydrothermal porphyry copper mineralization in the Ahar. In this research to remove atmospheric and topographic effects from ASTER data, the log-residual method (LRM) was used. Four methods, Relative Band Depth Ratios (RBD), Principal Component Analysis (PCA), Minimum Noise Fraction (MNF) and matched filtering (MF), were used to processing and interpretation of remote sensing data in the study area. Results show that ASTER images provide preliminary mineralogy information and geo-referenced alteration maps at low cost and with high accuracy for reconnaissance porphyry copper mineralizations. 相似文献
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Melanie Brandmeier 《国际地球制图》2013,28(8):629-648
A combined approach to detect hydrothermal alteration zones and their mineral distribution is proposed for a relatively remote area around the Carhuarazo volcanic complex in southern Peru encompassing 2222 km2. In this region, tertiary volcanic structures associated with hydrothermal alteration are well known to host epithermal ore deposits. We make an attempt to detect and to quantify alteration minerals based on spectral analysis using ASTER reflectance data product provided by LP-DAAC. Besides commonly used ratio images, mineral indices (MI) and relative band depth images (RBD), we also extracted endmember spectra using Pixel-Purity-Processing preceded by minimum noise fraction transformation. These spectra are thought to represent the spectrally purest pixel of the image and show the typical absorption features of the main constituents. Based on this assumption, we used different spectral analysis methods in order to extract the most important alteration minerals for such an environment. These minerals were then used for matched filter processing in areas showing high values in MIs and RBDs. Using this method, we detected and mapped argillic alteration and variations in the distribution of important minerals like alunite, kaolinite or nacrite. There were no indications for the presence of propilitization at ASTER spatial resolutions. Our method can be applied easily to any ASTER scene and provides information about the intensity of alteration and the character of alteration zones. The intensity is highest in the centre of the Carhuarazo volcanic complex and is mostly argillic with a high content of alunite, dickite and other clay minerals. 相似文献