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. 6. A. Interpreted fluid-flow pattern within the detachment zone. High
fluid flow is restricted to intensely brecciated rocks leading to precipitation
of vein-filling iron oxides. By contrast, the relatively homogeneous marble is
pervasively impregnated by fine-grained goethite. See text for discussion. B.
Schematic diagram (not to scale) showing detachment fault–related mineralization in the roof of the Phyllite-Quartzite unit in western
Crete (for comparison, see Long, 1992, fig. 36).
Copyright © 2008 by Society of Economic Geologists
