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- W2360641114 abstract "This paper reports the SHRIMP U-Pb age of zircon from Tongshi magmatic complex in western Shandong. Eighteen analyses on zircon grains from porphyritic fine-grained diorite gave two concordant groups of ages, in which ten analyses presented ~(206) Pb/~(238) U ages from 167.9 Ma to 183 Ma with a weighted mean age at (175.7±3.8) Ma, and the other eight analyses provided ~(207) Pb/~(206) Pb ages from (2 502) Ma to 2 554 Ma with a weighted mean (2 518±11) Ma. Two analyses on zircon grains from syenite porphyry yield the ages of 2 485 Ma and 2 512 Ma, respectively. The age of (175.7±3.8) Ma indicates that the crystallization of Tongshi magmatic complex occurred in the middle Jurassic epoch. The age of (2 518±11) Ma is interpreted as the age of inherited magmatic zircon in Neo-archean Wutai period. According to the SHRIMP U-Pb data of zircon, the authors consider that there existed the early Yanshanian tectonic-magmatic thermal events in western Shandong, and the Guilaizhuang gold deposit related to Tongshi magmatic complex was formed between 170 Ma and 160 Ma." @default.
- W2360641114 created "2016-06-24" @default.
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- W2360641114 date "2004-01-01" @default.
- W2360641114 modified "2023-09-25" @default.
- W2360641114 title "THE SHRIMP AGE OF ZIRCON FROM TONGSHIMAGMATIC COMPLEX IN WESTERN SHANDONGAND ITS GEOLOGICAL IMPLICATIONS" @default.
- W2360641114 hasPublicationYear "2004" @default.
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