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- W2382205534 abstract "The in-situ zircon U-Pb dating revealed that the gabbro-diorites from Zibo and Linqu in Northwestern Shandong were formed at 128±2 Ma and 132±1 Ma,respectively.They are contemporary with the extensive Early Cretaceous magmatism in Western Shandong as results of the lithospheric thinning underneath the North China Craton(NCC).In comparison with the contemporaneous Jinan and Zouping gabbros,the Zibo and Linqu gabbro-diorites have notable higher zircon e Hf(t)(-5.9～-2.5 and-2.5～+3.2,respectively) and younger zircon Hf model ages(876～1003 Ma and 639～867 Ma,respectively),suggesting a large contribution of the asthenosphere to the magmatism at Zibo and Linqu areas.Overall,the source of the Early Cretaceous mafic intrusions in the north of Western Shandong was dominantly old lithospheric mantle of the craton's interior.From the NCC's interior to the Tan-Lu fault,the zircon e Hf(t) values of the Early Cretaceous mafic intrusions change from strong negative to less negative or slightly positive,indicating the increased participation of asthenosphere for the magmatism.The Tan-Lu fault should have been an important weaken lithospheric zone responsible for the spatial and temporal heterogeneous of the Early Cretaceous mafic magmatism in Western Shandong." @default.
- W2382205534 created "2016-06-24" @default.
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- W2382205534 date "2012-01-01" @default.
- W2382205534 modified "2023-09-23" @default.
- W2382205534 title "Spatial Variation of Zircon Hf Isotopes for the Early Cretaceous Mafic Intrusions in Western Shandong and its Genesis" @default.
- W2382205534 hasPublicationYear "2012" @default.
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