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Economic Geology; January 2005; v. 100; no. 1; p. 165-174; DOI: 10.2113/100.1.0165
© Society of Economic Geologists

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FIG. 1. A. Generalized geologic and tectonic map of western Crete (modified from Creutzburg et al., 1977; and Kopp and Ott, 1977), showing the tectonic units, the detachment fault, and the two major iron-oxide deposits, located in the roof of the Phyllite-Quartzite unit. B. and C. Detailed geologic maps and cross sections of the Kakopetros and Ravdoucha iron-oxide deposits. Note vertical exaggeration of the cross sections.

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