金矿为浅-中深成矿的中温热液矿床。
The deposit is a mesothermal gold deposit mineralized in shallow middle depth.
矿石矿物组合显示中—低温成矿特征，成矿温度、压力及成矿深度也均反映出矿床具低温浅成特征。
The ore and mineral assemblage show the characteristics of low-to-moderate temperature, Besides, the ore-forming temperature, pressure and depth also reveal the epithermal feature.
通过焦家深部金矿床和浅部金矿床对比研究，揭示了新的金矿成矿规律：浅部金矿床和深部金矿床之间为无矿间隔或弱矿化带；
Some new gold metallogenic law be revealed by comparative study for shallow and deep gold deposits. There is ore-free interval or weak mineralized zone between shallow and deep gold deposit.
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