吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (4): 1090-1103.doi: 10.13278/j.cnki.jjuese.20180230
• 地质与资源 • 上一篇
张健, 张德军, 郑月娟, 陈树旺, 张海华, 苏飞, 黄欣
Zhang Jian, Zhang Dejun, Zheng Yuejuan, Chen Shuwang, Zhang Haihua, Su Fei, Huang Xin
摘要： 为厘清内蒙古林西县会长地一带出露的一套生物化石匮乏的砂砾岩组合的地质时代、地层归属及其碎屑物质来源，进而探讨西拉木伦河缝合带的形成演化，对研究区砂岩样品进行了碎屑锆石LA-ICP-MS U-Pb年代学研究。测试结果主要分布在6个年龄区间：（285±4）~（246±4） Ma （峰值为264 Ma）、（317±5）~（293±4） Ma （峰值为310 Ma）、（610±10）~（344±6） Ma （主峰值为423 Ma）、（992±14）~（907±13） Ma、（1 467±18）~（1 424±22） Ma、（1 948±14）~（1 768±16） Ma，另具3颗年龄分别为（1 171±17）、（1 238±17）和（2 443±31） Ma的锆石。锆石CL图像与Th/U值共同指示绝大多数锆石为岩浆结晶锆石。264 Ma的峰值年龄限定了地层的沉积下限为晚二叠世，应属林西组；沉积物源区示踪显示砂岩沉积时具佳蒙板块（北方地块群）与华北板块两个物源区，指示佳蒙板块（北方地块群）与华北板块于晚二叠世时已拼合，拼合位置为西拉木伦河一线。
中图分类号:
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