吉林大学学报(地球科学版) ›› 2017, Vol. 47 ›› Issue (3): 719-733.doi: 10.13278/j.cnki.jjuese.201703107
张艳1, 韩润生1, 魏平堂2, 邱文龙1
Zhang Yan1, Han Runsheng1, Wei Pingtang2, Qiu Wenlong1
摘要: 通过会泽矿山厂铅锌矿床闪锌矿流体包裹体显微测温和成矿物理化学条件参数计算,结合前人研究结果,得出以下认识:会泽矿山厂铅锌矿床闪锌矿流体包裹体均一温度为126~280 ℃,具有较宽的变化区间,盐度(w(NaCl))为3.2%~22.8%; 白云石流体包裹体均一温度为86~163 ℃,大部分盐度较低,为1.1%~14.8%。3个成矿阶段闪锌矿和白云石中流体包裹体均一温度和盐度具有较明显的分布特征:从热液成矿期I阶段→Ⅱ阶段→Ⅲ阶段→围岩蚀变,流体呈现中高温-高盐度→中温-中高盐度→中低温-中高盐度→中低温-低盐度的演化规律。在整个热液成矿过程中,有两种不同盐度的流体参与了作用,流体混合可能是矿物沉淀的主要机制。pH值计算结果表明,迁移阶段时,成矿流体呈酸性,从成矿阶段I—IV,流体pH逐渐增大,主成矿阶段II—III时,闪锌矿和方铅矿在中性、弱碱性下大量析出。受控于CO、CO2、O2间逸度平衡的CO2-3和HCO-3缓冲对调节了成矿流体的pH值,碳酸盐岩在铅锌的运移沉淀中起了至关重要的作用。
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