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ZlateHory块状硫化物矿床区域内的镁铁质变质火山岩被解释为是经受了绿片岩相变质作用的聚合板块边缘的玄武岩和玄武质安山岩。根据主要元素和微量之素组份,这些变质基性岩显示为岛弧拉斑玄武质到低钾、钙—碱性组成。所研究近50％的镁铁质变质火山岩样品,在球粒陨石标准化的稀土元素模式中具显著的Ce负异常。Ce衰减绿片岩是岛弧拉斑玄武质组份的变质基性岩热液蚀变表现,蚀变伴有硫化物矿化作用。这从Ce衰减岩石中,Ba和S共同富集与Ce/Ce值和CO_2高含量的相互关系得到指示。Ce异常可能由成矿蚀变、海水衍生的溶解作用引起。Ce衰减绿片岩的产生,支持了兹拉特霍尔区域内矿床的火山成因说。
Mafic metamorphic volcanics within the Zlatehory massive sulphide deposits are interpreted as basalts and basaltic andesite margins at the margins of polymerized platelets that underwent metamorphism. According to the major elements and trace elements, these metamorphic basic rocks are characterized by island arc pull-out basaltic to low potassium and calcium-alkaline compositions. Nearly 50% of the mafic metamorphic volcanic rocks studied have significant Ce negative anomalies in the normalized REE patterns of chondrules. Ce-decadal greenschist is a metamorphic basement hydrothermal alteration of the basaltic component of the island arc pullout with alteration associated with sulfide mineralization. This indicates that the correlation between the co-enrichment of Ba and S with the Ce / Ce value and the high CO 2 content in Ce-attenuated rocks. The anomaly of Ce may be caused by alteration of mineralization and dissolution of seawater. The Ce-attenuated greenschists have supported the volcanism of the deposits in the Zlatöhl region.