Characteristics of ore-forming fluid and sources of ore-forming material in the Yangzhaiyu gold deposit, Xiaoqinling gold district

• The Yangzhaiyu gold deposit is an orogenic-type deposit. • Ore-forming fluid: medium-high temp., low-sal., CO 2 -rich, CO 2 –H 2 O–NaCl system. • Fluid evolution driven by multi-source mixing from crust-mantle interactions. The Yangzhaiyu deposit is a large lode gold deposit in the Xiaoqinling region, along the southern margin of North China Craton, and it occurs mainly in the deep metamorphic gneiss series of the Taihua Supergroup. Researches based on petrography, micro-thermometry and Laser Raman analysis suggest that the homogenization temperature of ore-forming fluid was 216–346 ℃, the salinity was 6–8.7 %, with corresponding average density of 0.72–0.9 g/cm 3 . The ore-forming fluid was medium–high temperature, low salinity, CO 2 -rich, and belonged to the CO 2 –H 2 O–NaCl system. From stages I to IV, the metallogenic temperature, salinity and pressure showed a decreasing trend. Fluid immiscibility may be the precipitation mechanism of native gold in the Yangzhaiyu gold deposit. The H–O isotopic values of fluids (δD H2O = – 61 to – 51.8 ‰, δ 18 O H2O = 2.7 to 6.9 ‰) in stage I to IV suggest that the ore-forming hydrothermal fluid may have been a multi-source mixed hydrothermal fluid such as metamorphic water, magmatic water and meteoric water, which was mainly derived from metamorphic water and magmatic water, meteoric water gradually added with the mineralization process. The He–Ar isotopic values of fluids ( 3 He/ 4 He = 0.63–1.2 Ra, 40 Ar/ 36 Ar = 3978.6–5044.9) in stage I to IV suggest that the ore-forming fluid was a mixture of mantle source and crust source, mainly crustal source helium. With the progress of mineralization, the proportion of mantle source helium in the ore-forming fluid gradually decreases. The S isotopic values of sulfide (δ 34 S V-CDT = – 3.7 to 4.7 ‰, δ 34 S ∑s = – 5.4 to 4.5 ‰) in stage I to IV suggest that δ 34 S consistent with the characteristics of mantle-derived sulfur and the ore-forming sulfur may come from the Taihua Supergroup. The Pb isotopic values of sulfide ( 206 Pb/ 204 Pb = 17.015–17.158, 207 Pb/ 204 Pb = 15.394–15.524, 208 Pb/ 204 Pb = 37.481–37.91) in stage I to IV suggest that the ore-forming fluid was deep source mixed Pb from the mantle and the crust. The source of Pb in the deposit could be the Taihua Supergroup. The main mechanism of ore-forming fluid evolution was that the deep-source ore-forming fluid produced by crust-mantle interaction mixed with metamorphic hydrothermal fluid, meteoric water and other source fluids during upward migration in multiple stages during the whole ore-forming period. According to the geological, tectonic environment, fluid inclusions and isotopic data, combined with previous studies, the Yangzhaiyu gold deposit is considered as an orogenic gold deposit.