The topographic features and the boundary of the geological units can be observed in the structural features of satellite images in the brightness changes of the spectra. Many of the interesting geological structures are very small in size compared with the minimum scale of the satellite images which is represented as pixel which is the spatially minimum size of observation, though the scales are not enough to detect the detailed structures related to mineral deposits. Pattern recognition by computer is a possible method to study digital images to detect structures on the surface. In this study, the structures in images are divided into linear, textural, and spectral patterns, then integrated together in the island arc areas in a tropical region of Indonesia in order to analyze the relationship of the images to mineral deposits.
Lomblen Island in the Lesser Sunda Islands was chosen to be studied because of some peculiar ring structures and the characteristic arrangement of the long axis of the island in the direction northeast to southwest. The ring structure is possibly a volcanic cauldron which are related to the epithermal ore deposits in many areas.
Four types of edges are generally considered as step, tilt, roof, and line. The form of line is suggested by the arrangements of three or more pixels with characteristic intensities along straight or quasi-straight lines. The parallel arrangement of pixels with distinctively different intensities is easily detected as a line. Because the digital image often includes noise, the effect of noise is frequently eliminated from the original image using averaging of intensities between the neighboring pixels or other processes. Some topographic features are observed by the areal change of the brightness of sunlight. The areal change of images can be measured by their textural quantity. There are many methods of texture extraction. The rudimentarily textural quantity is the standard deviation of the brightness in a specific area. The standard deviation of brightness indicates topographic changes which respond to the contrast or change of brightness in images. The density calculation has the effect to average the areal value, the result in this study is ambiguous like the standard deviation image.
We found mineralized zones in separated areas of northern Lomblen Island. In northwest point of the ring structure, the silicified veins contains up to 2.0 ppm silver in a manganese oxide zone. In the northeast point of the ring structure, quartz and barite veins contain up to 4.2 ppm gold with several tens of ppm silver and copper and zinc sulfide. There is up to 687 ppm gold in the weathered quartz vein. High gold samples in quartz veins contain about 20 ppm gold locally. According to gravity measurements, the rim of the ring structure has very low gravity values whereas the central mountain area of the ring structure has high gravity. We suggest that the area of the ring structure could be a resurgent cauldron which are frequently related gold-silver deposits.
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