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Romania The Apuseni Mountains (West Romania) enclose many andesitic intrusions Some of these intrusions are associated with porphyry copper and/or epithermal ore deposits This study focus on the Bolcana area where a spatial association is observed between a porphyry copper (Bolcana, Cu +/-Au) and several low-sulfidation epithermal deposits (Troita, Pb- Zn; Magura, Au) A rather complete sampling was obtained in mine, open-pit and at surface. Studies of the veins geometry, mineralogy, fluids and alterations were carried out to highlight the relation between all these deposits : only spatial or a possible genetic one ? -A 3D geometry study using the GOCAD software (©2004, Earth Decisions Sciences) shows that the various ore deposits are spatially organised around the porphyry copper, with the Pb-Zn epithermal deposits close to the porphyry copper and the Au ones more in periphery. These spatial organisation excludes collapse events. -The porphyry Cu-Au mineralisation is represented by chalcopyrite, pyrite, bornite, magnetite, hematite, molybdenite, with subordinate gold (mainly as inclusion in chalcopyrite) The epithermal mineralisation consists of pyrite, sphalerite, galena, chalcopyrite, tetrahedrite, bournonite, marcasite, native gold, asenopyrite and pyrrhotite. -The nature of the rock alterations was determined by X-ray diffraction on whole rock samples. Its spatial localisation allows the visualisation of the sphere of influence of hydrothermal fluids, Fluid inclusion studies, made on a profile between the porphyry and the epithermal deposits, express the physical and chemical evolution of the characteristics of fluids. Results give evidence of a continuity of the different studied parameters and suggest a genetic relation between all the deposits ,
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TiO 2 , P 2 O 5 ) sont analysés par ICP-AES. La perte massique après chauffage correspond à la perte au feu. Le spectromètre est un spectromètre d'émission plasma à couplage inductif (Jobin Yvon JY 70 type II), p.222 ,