Hou, Lin, Peng, Huijuan, Iriondo, Alexander, Zhou, Qi, Ding, Jun, Guo, Yang, Guo, Linnan, Xu, Siwei, and Zeng, Xiangting
Garnet is an important metasomatic mineral in iron oxide-copper–gold (IOCG) ore systems, but its crystallization mechanisms and relationship to fluid evolution in IOCG are poorly understood. The Yinachang deposit is a typical IOCG deposit in the Kangdian region, southwest China. Zoning of the deposit include a breccia zone, a K-Fe alteration zone which can be subdivided into proximal and intermediate zones, and distal Na alteration zone. Iron ore bodies occur both in the breccias and in the meta -clastic rocks of the Yinmin Formation, and are replaced or cut by later Cu-Au-bearing layers and veins. The sequence of events include pre-ore Na±Fe alteration (stage 1), K-Fe±REE mineralization (stage 2), Cu±Au mineralization (stage 3), and barren veins (stage 4). Electron Probe Micro Analyzer (EPMA) and Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) analyses for garnets from the deposit were done to investigate the incorporation of trace elements into garnet, and to evaluate the potential of garnet mineralogy and geochemistry for understanding the ore-forming process of the IOCG ore systems. Garnets of the Yinachang deposit are hosted in the Fe-Cu ore bodies, proximal silicate alteration zones, and intermediate garnet-biotite-quartz zones. They are almandine-rich with lesser grossular and spessartine contents (Alm 65-78 Gro 5-17 Sp 5-17) and can be divided into three types. Type 1 garnets in the ore bodies (Grt 1) and type 2 garnets in the proximal silicate alteration zones (Grt 2) are pink to purple, euhedral to subhedral coarse grains. Grt 1 have core-rim texture, and Grt 2 have alteration of chlorite and are mainly crosscut by ore-bearing veins. They are both extremely large ion lithophile elements (LILEs)-depleted and enriched in high field strength elements (HFSEs), and have low total rare earth element (∑ REE) contents, but variable light (L) REE vs heavy (H) REE ratios (Grt 1: LREE-enriched and variable Eu anomalies; Grt 2: HREE-enriched and irregular REE patterns with positive Eu anomalies). Type 3 garnets in the intermediate garnet-biotite-quartz zones are purple-brown, inclusion bearing, relatively small anhedral grains that have higher LILE, HFSE, and ∑REE contents, and exhibit LREE-depleted and HREE-enriched patterns, with marked positive Eu anomalies. Based on geological and mineralogical obervation, we interpret that these three types of garnets are hydrothermal in origin and were formed during alteration and mineralization, but were controlled by different mechanisms due to different growth environment. Formation of Grt 1 and Grt 2 were mainly related to a substitution mechanism controlled by the crystal chemistry, physicochemical conditions of the closed hydrothermal system, and buffering effects of carbonate wall rocks during slow infiltration metasomatism, whereas formation of Grt 3 appears to be controlled mainly by surface adsorption and related to the composition of external fluid such as meteoric water during later rapid garnet growth. A decrease in temperature, pressure, and f O2 triggered by mixing of two fluids, as inferred from previous fluid inclusion studies, might have been responsible for the distinct mineralogical and geochemical characteristics of the three types of garnets. Garnets from IOCG deposits around the world showed various textual and geochemical characteristics. Generally, almandine and andradite are dominating end members for IOCGs. Andradite is typical for metasomatic origin, but the origin of almandine is still controversial. Although almandine garnet is generally considered to form during metamorphism, the occurrence of hydrothermal almandine in the alteration zones of IOCG deposit could reveal the metasomatism between Fe-bearing fluid and Al-enriched pelite protolith in a sufficiently reduced environment. It could also be possible that the metasomatism during mineralization has enriched the protolith with Fe, and the post-ore metamorphism formed almandine by providing high temperature and pressure. Additional mineralogical and geochemical studies of the garnets in IOCG deposits are needed to determine the relationship between garnet crystallization and specific episodes of ore-forming process or post-ore metamorphism. [Display omitted] • Three types of garnets with varied mineralogical and geochemical characteristics are identified from different mineralization and alteration zones in the Yinachang deposit. • Garnet growth in the Yinachang deposit was controlled partly by crystal chemistry and growth kinetics, but largely by external factors (i.e., fluid and host rock composition, T, P, and f O 2 , and diffusive versus advective metasomatism). • Almandine could be of metasomatic origin if a Fe-bearing hydrothermal intensively react with Al-enriched pelite protolith in a sufficiently reduced environment. Garnet is an important metasomatic mineral in iron oxide-copper–gold (IOCG) ore systems, but its crystallization mechanisms and relationship to fluid evolution in IOCG are poorly understood. In this study, major and trace element analyses were conducted on garnets from the Yinachang IOCG deposit in the Kangdian region, southwest China, in order to reveal their characteristics and forming process. Garnet commonly occurs in the K-Fe ± REE mineralization stage and Cu ± Au mineralization stage of the Yinachang deposit. Three types of garnets are identified from this deposit, which generally have high almandine but low grossular and spessartine contents (Alm 65-78 Gro 5-17 Sp 5-17). The type 1 garnet (Grt 1) in the ore bodies and the type 2 garnet (Grt 2) in the proximal silicate alteration zones are pink to purple, euhedral to subhedral grains. Grt 1 exhibit zoning pattern, and Grt 2 were altered into chlorite and was mainly crosscut by ore-bearing veins. They are both extremely depleted in LILEs and enriched in HFSEs, with low total rare earth element ∑ REE contents but variable LREE vs HREE ratios. The type 3 garnets (Grt 3) in the intermediate garnet-biotite-quartz zones are purple-brown, anhedral grains with high LILE, HFSE, and ∑ REE contents, and exhibit LREE-depleted and HREE-enriched patterns, with marked positive Eu anomalies. All three types garnets that formed during alteration and mineralization are hydrothermal, but their composition is controlled by different mechanisms due to different environments. Compositions of Grt 1 and Grt 2 are mainly related to substitution mechanism controlled by crystal chemistry, physicochemical conditions of the closed hydrothermal system, and buffering effects of carbonate wall rocks during slow infiltration metasomatism, whereas the composition of Grt 3 is mainly controlled by surface adsorption and related to the composition of external fluid during later rapid garnet growth. Decreases in temperature, pressure, and f O 2 triggered by mixing of fluids could be responsible for the distinct mineralogical and geochemical characteristics of the three types of garnets. Garnets from IOCG deposits show various textual and geochemical characteristics worldwide. Generally, almandine and andradite are dominating end members for IOCGs. Andradite is typical for metasomatic origin. Although almandine garnet is generally considered to form during metamorphism, the occurrence of hydrothermal almandine in the alteration zones of IOCG deposits reveal a metasomatism between Fe-bearing fluid and Al-enriched pelite protolith in a sufficiently reduced environment. Also, it is possible that the metasomatism during mineralization has enriched the protolith with Fe, and the post-ore metamorphism formed almandine by providing high temperature and pressure. [ABSTRACT FROM AUTHOR]