四川大渡河谷灯影期层状铅锌矿床中震积岩的发现及其成矿意义
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摘要
在四川大渡河谷震旦纪灯影期热水沉积大型层状铅锌矿床中,作者发现了较典型的震积岩序,包括震裂角砾岩、震塌角砾岩(矿)、震褶岩(矿)、震积角砾岩(矿)、震积不整合、层内断层等震积岩及震积构造,估计震裂岩的分布面积达1000km2以上.震积岩与热水沉积黑色硅岩及铅锌矿层呈同期、同位产出,它们之间存在内在的成因联系.作者经研究认为,大渡河谷地区在晚震旦世末期曾发生一次强烈的海底地震及多幕相对较弱的余震,海底地震可能是诱发深部含矿流体向汉源-峨眉北东东向同沉积凹陷轴部的断裂带汇集、运移并喷溢出海底形成大规模层状铅锌矿床的动力学机制.铅锌矿床中震积岩的发现具有重要的意义,为研究地震灾变事件与有色金属成矿作用的关系提供了重要实例.
引文
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