吉林省“大黑山条垒带”晚古生代火山事件及其构造意义

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对出露于吉林省"大黑山条垒带"、行政区辖属伊通县发展乡一带的"大黑山火山岩"-安山质凝灰熔岩、片理化流纹岩分别采样并挑选锆石,经LA-ICP-MS定年,查明安山质凝灰熔岩74颗锆石的~(206)Pb/~(238)U年龄介于1 873~240 Ma,其中~(206)Pb/~(238)U年龄值介于317~240 Ma的69粒锆石均显示出岩浆成因特征,表明研究区自晚石炭世晚期便存在火山事件,火山喷发活动于早、中二叠世发展至峰期,该火山岩形成于晚石炭世晚期至晚二叠世,并于早、中三叠世遭受了岩浆作用;古元古代
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