2003
DOI: 10.1080/0143116021000023862
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Mapping the Nidar Ophiolite Complex of the Indus Suture Zone, Northwestern-Trans Himalaya using IRS-1C/1D data

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Cited by 14 publications
(7 citation statements)
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“…This method, based on a principal component transformation of the acquired data, is widely applied and has been discussed by Nasir (2015, 2013), Philip et al (2003), Matthews and Jones (1992), Abrams et al (1988), Rothery (1984), and Gillespie et al (1986). In the present study, the transformed channels were contrast stretched and arbitrarily assigned primary colors for display as a color composite image.…”
Section: Image Analysis and Interpretationsmentioning
confidence: 99%
“…This method, based on a principal component transformation of the acquired data, is widely applied and has been discussed by Nasir (2015, 2013), Philip et al (2003), Matthews and Jones (1992), Abrams et al (1988), Rothery (1984), and Gillespie et al (1986). In the present study, the transformed channels were contrast stretched and arbitrarily assigned primary colors for display as a color composite image.…”
Section: Image Analysis and Interpretationsmentioning
confidence: 99%
“…Although previous studies have demonstrated the capability to improve lithological classification accuracies through data integration, they have been confined to using data with only moderate-to-coarse spatial resolutions (i.e., 12.5-30 m). The potential to delineate lithological contacts in finer detail and with better accuracy is further enhanced by the availability of high-resolution remote sensing data (Philip et al, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…For these reasons lithological maps are typically generated using limited numbers of field and outcrop observations which may, as a consequence, result in some concern regarding the accuracy of the lithological contacts (Philip et al, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…In addition to this, there are a number of faults, which have been confirmed by earlier workers. Traces of faults-fractures-joints which are identifiable on the digitally enhanced (Philip et al 2003), standard false-colour composite of LISS IV data, have been mapped as the inferred lineaments in the study area. In order to understand the influence of tectonically active regional geological structures like the MBT and that of other structures towards slope destabilisation, distance to the confirmed thrusts-faults (Suzen 2002), distance to the inferred lineaments, as well as, the density of all the geological structures together have been prepared as raster GIS database with 25-m cell size.…”
Section: Causal Factors and Landslide Databasementioning
confidence: 99%