The hydrothermal process that led to the deposition of epigenetic sulfide mineralizations (mostly Fe-Cu sulfides) in the ophiolite of Oman appears to be closely related to successive orogenic movements. Vertical (diapiric) uplift of peridotite, along the axial trend of the mountains of Oman, resulted from pressure exerted during the counterclockwise movement and subduction of the Arabian plate during the Miocene to Recent periods. The ophiolite rocks previously were present in an oceanic rift, a part of an island arc in the Tethys ocean. The continuous movement of the plate also resulted in the rotation of the Oman mountains from a NW trend in the southeastern portion to a WNW trend along Jabal Akhdar, then NW, and finally to a N-S orientation in the northwestern portion. Lasail, Aarja, Bayda, and all other prospects in this study that contain Fe-Cu sulfide mineralization are located near or around either end of faults (discontinuities) that segmented the mountains of Oman. They also are found in silicified shear-tension fractures and jasperoid (quartzitic) dikes, veins, and veinlets trending NW, NNW, or NE (i.e., parallel to the trend of the mountain axis or to the directions of the gabbroic-diabasic sheeted dikes); these structures cut across hydrothermally altered pillow lavas, lava flows, gabbro, and peridotite. Beyond the mineralized zones, all these rock types–including the pillow lavas (greenschist and zeolitic facies)–are barren and devoid of any showing of sulfide mineralization; however, they are hydrothermally altered. Many fractured and sheared mineralized outcrops exhibit Fe-Cu oxidation products (gossans). It is thought that these mineralized cross-cutting structures predate the emplacement of ophiolitic rocks. Sedimentary stratabound sulfides overlying mineralized volcanics, such as those in Cyprus, are missing in Oman. Drilling core sections, mineralized with sulfides in lava flows, pillow lavas, and andesitic rocks, also are hydrothermally altered and alternate with fresh sections at Lasail, Aarja, Bayda, and other prospects. The massive sulfide sections commonly exhibit unreplaced volcanic relicts, indicating that the alteration succeeded the formation of rocks. Drill cores also reveal that the massive ores gradually changed to blebs and stringers, and then to disseminated ores, confirming the occurrence of replacement-type deposits (at 300° to 500° C). In our opinion, the high pressure involved in the circulation of the hydrothermal and ore-bearing liquids was exerted by successive uplifting and rotational orogenic movements on convective hot seawater of normal salinity and pH = 3. The concentration of Cu averages 60 ppmw in three olivine grains (from three peridotites) and 41 ppmw in high-MgO-high-Al2O3 basalts. Therefore, Cu, which averages 10,500 ppmw (from 12 prospects and the Lasail samples), could be only partially derived from peridotite, gabbro, and basalt. The copper is believed to be mostly magmatic in origin (from S-undersaturated komatiitic/picritic magma?) and to have been carried, together with Fe and S, by magmatic superheated (over 400° C) vapor plumes, which joined the hydrothermal convective seawater. Zinc, on the other hand, averages about 380 ppmw (without Lasail) and may have been derived mostly from pyroxenes. Zinc averages 31 ppmw in three lithospheric peridotites, 29 ppmw in lherzolite olivine, and 526 ppmw in the high-MgO-high Al2O3 basalts. The hot liquids (300° to 400° C) were convective seawaters (of normal salinity) that filtered down through fractures generated by the orogenic movements, were heated, mixed with magmatic superheated Cu-Fe-S-bearing vapor plumes, and probably leached out minor amounts of Zn, Pb, Ag, and Au from ophiolitic rocks (mainly gabbro and basalts). The base metals were transported as chloride complexes and reacted thereafter with S= to form sulfides during the upsurge and cooling of hot liquids. The filtering of the hydrothermal and ore-bearing liquids was forceful under the pressure of the successive orogenic movements.
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