Key points are not available for this paper at this time.
The Sierrita-Esperanza porphyry copper complex is central to a large fossil hydrothermal system located in the southeastern part of the Sierrita Mountains, Arizona. Abundant, closely spaced fractures exert a profound control of sulfide minerals and alteration in the mineralized center of the system. The extent and limits of the hydrothermal system in peripheral areas have been defined in this study by determination of the distribution and abundance of the altered and mineralized fractures. Mapping of these elements to their limit of occurrence has resulted in recognition of an area of about 60 km 2 where fractures related to porphyry copper mineralization occur and a contiguous area of about 40 km 2 where slightly older altered fractures, related to the first stages of Laramide igneous activity in the region, are present. Within the orebody, distinctive fracture types, as recognized by fracture style and alteration assemblages, occur in a consistent paragenetic succession. This same succession has been recognized in the areas peripheral to the pits but with variations for each alteration type as influenced by wall-rock mineralogies. The establishment of a sequence of vein alteration, commencing with quartz-orthoclase alteration, passing through precipitation of quartz and
Titley et al. (Tue,) studied this question.