Formation Age of the Sujiagou Komatiites in Western Shandong: Further Constraints from SHRIMP U-Pb Zircon Dating on Granitic Dykes

Formation Age of the Sujiagou Komatiites in Western Shandong: Further Constraints from SHRIMP U-Pb Zircon Dating on Granitic Dykes
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This paper is to honour Academician Li Tingdong, on the occasion of his 90th birthday (2020), who has made great contributions to geology in China. We thank Yang Chun, Zhang Zhichao and Zhou Liqing for mount making and zircon CL imaging. We also appreciate the technical support of Liu Jianhui and Che Xiaochao for the smooth operation of the SHRIMP instrument during zircon dating. Thanks are also to Yang Chonghui and Wang Xiaolei for helpful comments. This study was financially supported by the Key Program of the Ministry of Land and Resources of China (DD20190370, DD20190009, DD20190358, DD20190003).

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    Komatiites are presented as direct evidence for higher mantle temperatures during the Archean. In the North China Craton, komatiites with spinifex structure have been identified only at one locality, i.e. the Sujiagou area, western Shandong. They were considered as formed during the early Neoarchean mainly based on their association with supracrustal rocks considered to be that age. This study carried out SHRIMP U-Pb zircon dating on metamorphosed trondhjemitic and monzogranitic dykes intruding the Sujiagou komatiites, and they have magmatic zircon ages of 2592 ± 12 Ma and 2586 ± 13 Ma respectively. This provides direct evidence that the komatiites formed during the early Neoarchean.

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WAN Yusheng, DONG Chunyan, XIE Hangqiang, WANG Shijin.2020. Formation Age of the Sujiagou Komatiites in Western Shandong: Further Constraints from SHRIMP U-Pb Zircon Dating on Granitic Dykes[J]. ACTA GEOLOGICA SINICA(English edition),94(4):877~883

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  • 收稿日期:2020-04-05
  • 最后修改日期:2020-06-05
  • 在线发布日期: 2020-08-25
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