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Titlebook: Remote Sensing Geology; Ravi Prakash Gupta Textbook 19911st edition Springer-Verlag Berlin Heidelberg 1991 Remote Sensing Applied Geology.

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書目名稱Remote Sensing Geology
編輯Ravi Prakash Gupta
視頻videohttp://file.papertrans.cn/827/826891/826891.mp4
圖書封面Titlebook: Remote Sensing Geology;  Ravi Prakash Gupta Textbook 19911st edition Springer-Verlag Berlin Heidelberg 1991 Remote Sensing Applied Geology.
描述There has been phenomenal growth in the field of remote sensing over the last two to three decades. It has been applied in the fields of geology, mineral exploration, forestry, agriculture, hydrology, soils, land use etc. - that is, in all pursuits of sciences dealing with the features, processes, and phenomena operating at the earth‘s surface. The status of geological remote sensing has rapidly advanced and the scientific literature is scattered. The aim of the present book is to systematically discuss the specific requirements of geological remote sensing, to summarize the techniques of remote sensing data collection and interpretation, and to integrate the technique into geoexploration. The main conceptual features of the book are: - To combine various aspects of geological remote sensing, ranging from the laboratory spectra of minerals and rocks to aerial and space-borne remote sensmg. - To integrate photogeology into remote sensing. - To promote remote sensing as a tool in integrated geoexploration. - To elucidate the wide-spectrum geoscientific applications of remote sensing, ranging from meso- to global scale. The book has been written to satisfy the needs of mainly graduate
出版日期Textbook 19911st edition
關鍵詞Remote Sensing Applied Geology; exploration; geology; geoscience; hydrology; mineral; remote sensing; miner
版次1
doihttps://doi.org/10.1007/978-3-662-12914-2
isbn_ebook978-3-662-12914-2
copyrightSpringer-Verlag Berlin Heidelberg 1991
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Physical Principlesaluable reviews on the nature of EM radiation and physical principles are given by Suits (1983), Fraser and Curran (1976) and Silva (1978). The properties of the EM radiations can be classified into two main groups: (1) showing wave nature and (2) showing particle characteristics.
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Interpretation of Data in the Thermal Infrared Regionct that in this region, radiations emitted by the earth due to its thermal state are far more intense than the solar reflected radiations (Fig. 9.1), and therefore any sensor operating in this wavelength region would primarily detect the thermal radiative properties of the ground materials.
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Interpretation of SLAR Imageryays down on the earth, transverse to the flight direction. It emits pulses of microwave energy, which illuminate long narrow strips on the ground. The back-scattered signal, sensed by the antenna, is recorded in order of arrival time. This yields a radar image.
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https://doi.org/10.1007/978-3-662-12914-2Remote Sensing Applied Geology; exploration; geology; geoscience; hydrology; mineral; remote sensing; miner
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Springer-Verlag Berlin Heidelberg 1991
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