The control of various combinations of fluid processes on Au-Te enrichment: Insights from the giant Dongping Au-Te deposit

• The control of various combinations of fluid processes on Te-Au enrichment in lode gold deposits. • Microtexture, trace element and in-situ δ 18 S analyses of three pyrite generations at Dongping. • Different degrees of fluid boiling, mixing and fluid-rock reaction control Te-Au enrichment in three generations. Te-rich gold ores are important potential targets for the Te recovery and their formation is usually the results of different fluid processes, including fluid boiling, mixing and fluid-rock interaction. However, how the various combinations of these processes control Te enrichment together with Au remains poorly understood. The giant Dongping Au-Te deposit in the North China Craton provides an excellent opportunity to investigate this question. Here, we present major, trace element, and S isotope compositions of three generations of pyrite (Py-1, Py-2a, and Py-2b) at Dongping, based on the detailed petrographic observations. The results show that Te and Au occur mainly as solid solution in pre-ore Py-1, distinct from their existence mostly in form of mineral inclusion in Py-2a of syn -ore veining stage. These two styles of occurrence are suggested for Py-2b in syn -ore disseminated gold ores. In addition, trace element mapping reveals a coupling characteristic between Te and Au. When combining the results presented here and previous data, such enrichment behaviors of Te and Au are proposed to be related to different degrees of various combinations of fluid processes. Pre-ore fluids forming Py-1 are under a condition of high temperature and f O2 , and thus contain high Te concentrations (HTeO 3 – and/or TeO 3 2– ) and low Au concentrations (Au(HS) 2 – ). Gentle boiling during the Py-1 formation decreased the loss of Te to vapor phase, thereby causing the co-enrichment of Te and Au in liquid-rich fluids. Meanwhile, high As concentrations facilitated the co-incorporation of Te and Au into Py-1 as solid inclusions. Vigorous fluid mixing at the onset of Py-1 formation cannot trigger the precipitation of Te because of high temperature and f O2 . HTe – and/or Te 2 2– are dominant for Te transport in reduced fluids of syn -ore stage. During the formation of Py-2a, a process involving Te-rich metallic melts scavenging Au from ore fluids could account for the co-enrichment of Te and Au. This process was activated by fluid oxidation caused by vigorous processes of fluid boiling and mixing. The deficient As concentrations likely led to the scarce occurrence of Te and Au as solid inclusions in Py-2a. The oxidation of fluids systems induced by igorous boiling and fluid-rock interaction was responsible for the co-enrichment of Te and Au in Py-2b, which also invoked Te-rich metallic melts. The moderate As concentrations may explain some Te and Au as solid solution in Py-2b.