2014
DOI: 10.30897/ijegeo.300739
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Morphologic Features of Kapıdağ Peninsula and its Coasts (NW-Turkey) using by Remote Sensing and DTM

Abstract: Although it is an inland sea, the Sea of Marmara and its surroundings have rather complex morphology due to the active tectonics of the North Anatolian Fault (NAF) zone in this region. The Kapıdağ Peninsula which is located at its southern coasts also represents a complex morphology. Macro morphologic units of Kapıdağ Peninsula are N-S trending deep valley systems, mountain areas and Belkıs isthmus. The most coastal area of peninsula has terraces, coastal plains and alluvial valley floors. These unique morphol… Show more

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Cited by 22 publications
(16 citation statements)
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“…Spectral indices, such as normalized difference vegetation index and band ratios can be effectively used to distinguish mangrove forests from water, mud flats and sand beach. However, terrestrial vegetation and watervegetation mixed pixels may complicate mangrove forest identification by using these spectral indices (GAzioğlu, et al, 2014;Tiezhu et al, 2016). The mangrove density distribution in Pongok Island was analyzed using the Normalized Difference Vegetation Index (NDVI) computed from Landsat data (Umroha, et al, 2016).…”
Section: Mangroves Health Assessment Using Remote Sensingmentioning
confidence: 99%
“…Spectral indices, such as normalized difference vegetation index and band ratios can be effectively used to distinguish mangrove forests from water, mud flats and sand beach. However, terrestrial vegetation and watervegetation mixed pixels may complicate mangrove forest identification by using these spectral indices (GAzioğlu, et al, 2014;Tiezhu et al, 2016). The mangrove density distribution in Pongok Island was analyzed using the Normalized Difference Vegetation Index (NDVI) computed from Landsat data (Umroha, et al, 2016).…”
Section: Mangroves Health Assessment Using Remote Sensingmentioning
confidence: 99%
“…Actively, as a source of energy for photosyhthesis, photosynthesizing leaves absorb the red wavelenghts (LANDSAT TM band 3) and reflect the short-wave infrared (LANDSAT TM band 4). The diffrence between the two is proportional to the amount of photosysthesis (Parodi, 2002;Schreiber, 2006;Gazioğlu, et al, 2014;İslam, et al, 2016;Gazioğlu, et al 2016;Avşar, et al, 2016;Osgouei and Kaya, 2017;Kaya et al, 2017). NDVI is unaffected by band sharpening since the relative contributions of the near-infrared and red bands remain unchanged by the fusion method (Wiemker, 1998).…”
Section: Processing Landsat Tm Imagerymentioning
confidence: 99%
“…Remοte sensing techniques are increasingly playing an impοrtant rοle in geοsciences for mineral exploration and of lithological discrimination (Sabin,1999;Rowan and Mars 2006;Rajendran 2011;Gazioğlu et al, 2014;Avşar et al, 2016;, İncekara et al, 2017;Shirazi et al, 2018;Zoheir et al, 2019). Based οn remοte sensing data such as Landsat TM, ETM+ and Aster have great potentials in geological interpretations.…”
Section: Introductionmentioning
confidence: 99%