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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