Lithogeochemical, mineralogical analyses and oxygen–hydrogen isotopes of the Hercynian Koudiat Aïcha massive sulphide deposit, Morocco

Abstract

Koudiat Aïcha is a Visean stratiform, volcanogenic massive sulphide (VMS) zinc-copperlead deposit, situated northwest of Marrakech, within the Central Domain of the Jebilet massif of the Western Moroccan Meseta. The Central Domain is formed mainly of sedimentary (argillite, siltstone, sandstone, carbonate) and magmatic (gabbro and rhyodacite) rocks that host numerous massive sulphide deposits (e.g., Koudiat Aïcha, Kettara and Draa Sfar) in a thick grayish argillite sequence (rhythmic metapelite). The deposit is stratabound and consists of highly deformed, sheet-like lenses of massive sulphide located structurally on the eastern flank of a large anticline. Prior to metamorphism, the country rocks were subjected to hydrothermal alteration which is particularly pronounced in the immediate vicinity of the sulphide deposits where chloritization and sericitization are prevalent. Hydrothermal alteration extends into both the stratigraphic footwall and the stratigraphic hanging wall. The footwall lacks an obvious pipe zone (sulphide stringers or vent complex) beneath the sulphide mineralization, but is characterized by an increase in the modal proportion of Mg-chlorite and by the breakdown of feldspar and sericite. Chloritization, the most extensive and readily recognizable alteration useful in mineral exploration, is evident for more than 60 m above the subcropping sulphide deposits. The hanging wall rocks show a pervasive sericitization (over 30 m wide) and a weak chlorite alteration accompanied by disseminated nodules of pyrrhotite stretched parallel to the S 1 foliation. Because chlorite and sericite are metamorphic minerals that also occur in unaltered rocks surrounding the sulphide deposits, abundant Mg-rich chlorite and the absence of feldspar in the footwall are used to distinguish hydrothermal alteration facies from metamorphic facies. The chlorite geothermometer reveals temperatures between 250 and 330 °C. Higher temperatures (up to 300 °C) are associated with chlorite located in and adjacent to sulphide mineralization, whereas lower temperatures correlate with distal chlorite in both the footwall and hanging wall rocks.Chemical trends in altered footwall rocks are shown by absolute mass gains for Fe 2 O 3total , MnO and MgO, by absolute mass losses for CaO, K 2 O and Na 2 O, and by a moderate loss in SiO 2 . Oxygen and hydrogen isotope compositions of Koudiat Aïcha lithofacies (6.2-12.4‰ for oxygen and −51‰ to −36‰ for hydrogen) have also been used to determine the temperature and origin of metalliferous fluids. The couple plagioclase-amphibole of gabbros provides equilibrium temperatures between 310 and 380 °C and suggests that the heat source for the ore-forming fluid system may have been igneous. On the other hand, oxygen and hydrogen isotope ratios cluster between normal values for sedimentary and magmatic rocks, suggesting a magmatic-metamorphic origin for the ore fluid.

Geologic, Hydrothermal, and Geochemical Relationships Between Bimodal Magmatism and Massive Sulphide Mineralization in the Central Jebilet-Guemassa Province (Western Moroccan Hercynides)

“…Total proven and probable resources are 3-5 Mt with average grades of 3 % Zn, 1 % Pb, and 0.6 % Cu (Lotfi et al 2010). …”

“…6). The present shape of the orebodies is controlled by a regional F 1 anticlinal megastructure and associated schistosity (Lotfi et al 2008(Lotfi et al , 2010, but the original lens-shaped geometry is largely retained.…”

“…Four main ore types are recognized: massive pyrrhotite ore, banded ore, Cu-rich massive sulphides and related stringer mineralization, and barren, rhythmically banded pyrrhotite interpreted to represent synsedimentary sulphide deposition (Ben Aissi 2008;Lotfi et al 2008Lotfi et al , 2010. However, inferred syngenetic relationships between black shales and massive sulphides are commonly obliterated by intense shearing.…”

“…In contrast, overall metal contents are consistently uniform between levels indicating little or no lateral zonation. Silver, Au, and Sn are concentrated at the top of the sulphide lenses and in adjacent hanging wall rocks (Lotfi et al 2010). Monoclinic pyrrhotite (up to 95 vol.%), sphalerite (7-8 wt% Fe), galena, and chalcopyrite are the main ore minerals, together with stannite, arsenopyrite, and pyrite.…”

“…Mass balance calculations indicate that hydrothermal alteration of the footwall host rocks was accompanied by pervasive leaching of K 2 O, Na 2 O, and CaO, moderate loss of SiO 2 , and precipitation of FeO, MgO, and MnO under a high-temperature regime (>150°C) and high water/rock ratios (>10). Conversely, sericite-and calcite-rich alteration of hanging wall rocks involved lower temperatures (<150°C) and atomic water-rock ratios (W/R) <5 Zouhry 1998;Ben Aissi 2008;Lotfi et al 2010;Rziki 2012).…”