My profile My library Metrics Alerts. Location map of the study area showing the tectonic map and the four intrusive ophiolite complexes of Mawat, Penjween, Pushtashan and Bulfat in Iraqi part of the Zagros Suture Zone modified after [ 6 , 9 , 11 ]. It is used to quantify the tectono-geomorphological variations, where high values represent highly deformed regions [ 47 , 81 ]. Shapefiles contain a single class of "vector" data such as points, lines, or polygons. This means that it may take a while to download these files, and that you will need a fast PC to work with them. The temperature of gabbro-diorite, conglomerate, clastic rocks and carbonite rocks are decreasing in the wavelength of We tested a set of SVMs using different combinations of input data chosen from 33 data layers. A wide spectrum absorptions region — nm centered in , a broad shallow feature — nm centered in , and a sharp spectrum absorptions in nm, nm and nm are due to olivine content [ 13 , 15 , 16 , 21 , , — ]. In addition, dunite containing chromite has a reflectance absorption in wavelength of nm, and nm, and gabbro sample has a reflectance absorption at a wavelength of nm, nm, nm, — nm and nm.
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Environment for Visualizing Images ENVI and PCI Geomatica software were used for data processing layer stack, subset, algebraic operations, radiometric correction, texture generation, filtering and classification. Environ , 91 , — Geophysics , 46 , — The Red beds series include four lithostratigraphic units which comprise silty shales, conglomerates, sandstones, marls, limestones and were deposited during the Tertiary [ 9 , 27 , 42 ]. The use of near-infrared spectroscopy to determine the degree of serpentinization of ultramafic rocks. The most suitable geomorphic feature is the surface index SI , a new and efficient index, which is able to map preserved and eroded portions of an elevated landscape at the same time [ 31 , 32 ]. SAM method does not consider the spectral illumination and only consider the spectral similarity between the reference and image spectra [ ], therefore it introduces potential commission errors in the results.
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Geographic Information Systems (GIS): Geospatial Data in Asia (beta)
Hyperspectral analysis of the ultramafic complex and adjacent lithologies at Mordor, NT, Australia. The chromite is coarsely crystalline and of greenish-black color embedded in the dunite host rock, Figure 12A. Then, we converted the Kelvin to Celsius temperature using Equation 4. A case study from Neyriz ophiolite, SW Iran. Landsat-TM-based discrimination of lithological units associated with the Purtuniq ophiolite, Quebec, Canada. Remote Sens , 50 , — Tectonic Geomorphology ; Wiley: New data and interpretations. Two thousand, seven-hundred, and twenty-seven test samples i. Articles 1—20 Show more.
Description:Arsalan Ahmed Othman prepared and accomplished the study. For the rest classes, the average overall reflectance of the carbonite and the clastics classes are higher than the conglomerate, and the valley fill sediments classes. The source of conglomerate is conglomerate of Red beds series. The shortening of the Zagros orogenic belt resulted from the ongoing subduction of the Arabian plate beneath the Eurasian plate [ 4 — 6 ]. The calibration file for the atmospheric correction was generated from the metadata of the ASTER scene. A coefficient of agreement of nominal scales. Metabasalt and basalt have reflectance absorption at a wavelength of nm and nm. This technique is able to select the pixels that are more pure by decreasing the maximum angle boundary.
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