Geology and genesis of gold deposits in the daduhe belt: A Case study of the Lianhua gold deposit on the Western margin of the Yangtze Craton, China

• There are two hydrothermal events in the Daduhe gold belt. • The metamorphic Kangding complex provided main fluids and ore-forming materials. • A magma related fluids was recognized from the orogenic Au deposit. The Daduhe gold belt (DGB) is an essential gold mineralization belts discovered in southwestern China. However, there are still some controversies on the material source, fluid origin and properties. The Lianhua gold deposit, as one of the typical gold deposits in the DGB, is suitable to understand the mineralization. Based on field investigation, and analysis on mineralogy, fluid inclusions, and S-H-O isotope geochemistry, a possible metallogenic model is proposed. According to field observations, the Lianhua deposit has experienced at least two phases of hydrothermal activity, namely, the ore-forming and post-ore periods. Three types of fluid inclusions are identified: 1) V CO2 –L H2O (C1 type), 2) V CO2±CH4 –L H2O (C2 type), and 3) V H2O –L H2O (W type). The inclusions in ore-forming periods are mainly C1 and C2 type, while the post-ore period is W type predominately. Microthermometric analyses show that ore-forming quartz veins formed in a low to medium temperature (201.6℃–315.2℃), low to medium salinity (3.05–13.20 wt% NaCl eqv.) H 2 O–NaCl–CO 2 ± CH 4 system. The H-O isotope of ore-forming quartz shows, the δ 18 O V-SMOW ranged from 7.29 ‰–10.81 ‰, whereas the δD V-SMOW ranged from − 63.5 ‰–−68.3 ‰, implying that the ore-forming fluids are formed by a mixture of metamorphic fluids and meteoric water. Fluid immiscibility caused by the separation of CO 2 ± CH 4 –H 2 O system and H 2 O–NaCl system may be the main mechanism of gold precipitation. The δ 34 S values of pyrite ranged from − 3.12 ‰–5.92 ‰, indicating that the Kangding complex provided ore-forming materials. The post-ore tourmaline quartz veins formed in a medium to high temperature (286.6℃–460.1℃), medium to high salinity (9.98–20.26 wt% NaCl eqv.) H 2 O–NaCl system. The δ 18 O V-SMOW is 9.16 ‰, whereas the δD V-SMOW is − 85.5 ‰, implying that the post-ore fluids are predominantly primary magmatic water or at least vast magmatic water injection. Tourmaline, as a characteristic mineral of post-ore hydrothermal event, is formed by crustal magmatic fluids reacted with the Kangding complex. However, the post-ore magmatic-hydrothermal fluids did not contribute to the enrichment of gold in the Lianhua deposit.