李光金,陈雷,庞科,汉春梅,阳乐,万斌,杨锋杰

• 1:山东科技大学地球科学与工程学院
• 2:青岛海洋科学与技术试点国家实验室
• 3:中国科学院南京地质古生物研究所和生物演化与环境卓越创新中心现代古生物学和地层学国家重点实验室

摘要(Abstract)：

近年来,鲁西地区拉伸系土门群中报道了大量与Rodinia大陆汇聚时间相一致的碎屑锆石,而与Rodinia大陆裂解相关的碎屑锆石非常少见。为此本文对鲁西地区寒武系底部李官组进行了LA-ICP-MS碎屑锆石U-Pb同位素测年。测试结果显示李官组碎屑锆石以古元古代碎屑锆石为主体,新元古代碎屑锆石次之,含三个峰值,分别为～756 Ma、～1872 Ma、～2532 Ma。依据地层接触关系以及化石特征,李官组被限定为都匀阶(～514—509 Ma)早期或稍早时期沉积,并可与辽南地区大林子组和淮北地区猴家山组下部进行对比,均为华北克拉通在寒武纪海侵初期最早沉积的一套碎屑岩地层。除～756Ma年龄峰值外,李官组碎屑锆石的年龄均可在华北克拉通找到对应的岩浆事件。依据李官组沉积时间、多数碎屑锆石对应的岩浆事件以及最新的古地理模型,华北克拉通很可能是李官组碎屑锆石的源区。～756 Ma碎屑锆石与Rodinia大陆裂解的时间一致,被解释为与裂解相关的岩浆活动在鲁西地区的记录。

关键词(KeyWords)： 华北克拉通;胶辽徐淮地区;鲁西地区;寒武纪;李官组;碎屑锆石

Abstract:

Keywords:

基金项目(Foundation): 国家重点研发计划(2016YFC0601001、2017YFC0603100);; 国家自然科学基金(41502019、41602007);; 中国科学院项目(XDB26000000、QYZDJ-SSW-DQC009);; 山东科技大学科研发展基金(2015YQJH102);山东科技大学研究生创新项目(SDKDYC190312)共同资助

作者(Author): 李光金,陈雷,庞科,汉春梅,阳乐,万斌,杨锋杰

DOI: 10.19839/j.cnki.dcxzz.2020.0014

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