In: Wagner W., Sz6kely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
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The thermal band algorithms, (12*14) / (13 2 ) and (14/13) /
(13/12) 3 were developed by considering the spectral responses
of mafic minerals exist in constituting rock units compared with
ASTER TIR bands. These algorithms are highly effective to
distinguish the olivine-rich ultramafic portions in the region of
ophiolitic rocks. It is also capable of mapping those lithologies in
a certain boundaries.
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