| 鲁西孟家屯一种细粒斜长角闪岩的锆石SHRIMP年代学 |
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| 关键词:western Shandong Fine-grained amphbolite chronology North China platform |
| 基金项目:原地质矿产部跨世纪人才基金项目;同位素开放实验室基金项目 |
| 作者 | 单位 | E-mail | | 杜利林 | 中国科学院地质与地球物理研究所,北京,100029,中国地质科学院地质研究所,北京,100037 | dulilin7310@sina.com | | 庄育勋 | 中国地质调查局,北京,100011 | | | 杨崇辉 | 中国地质科学院地质研究所,北京,100037 | | | 万渝生 | 中国地质科学院地质研究所,北京,100037 北京离子探针中心,北京,100037 | | | 王新社 | 中国地质科学院地质研究所,北京,100037 | |
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| SHRIMP U-Pb Zircon Chronology of Fine-grained Amphibolite in the Mengjiatun Area, Western Shandong |
| Based on studying mineral lithofaces, zircon characteristics and chronology, the authors obtained zircon SHRIMP metamorphic age of 2 604±11 Ma for fine-grained amphbolite from Mengjiatun area of western Shandong. According to metamorphic ages of Mengjiatun Formation and other magmatic ages of western Shandong, it is concluded that intense geological movement took place from 2 650 Ma to 2 600 Ma, which is quite different from other regions in the North China platform. Therefore western Shandong has its unique geological evolution history in Early Precambrian. |
| DU Li-lin,ZHUANG Yu-xun,YANG Chong-hui,WAN Yu-sheng,WANG Xin-she.2005.SHRIMP U-Pb Zircon Chronology of Fine-grained Amphibolite in the Mengjiatun Area, Western Shandong[J].Acta Geoscientica Sinica,26(5):429-434. |
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