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Volume 30 Issue 6
Dec 2019
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Article Contents
Zhaojun Song, Huimin Liu, Fanxue Meng, Xingyu Yuan, Qiao Feng, Dingwu Zhou, Juan Ramon Vidal Romaní, Hongbo Yan. Zircon U-Pb Ages and Hf Isotopes of Neoproterozoic Me-ta-Igneous Rocks in the Liansandao Area, Northern Sulu Orogen, Eastern China, and the Tectonic Implications. Journal of Earth Science, 2019, 30(6): 1230-1242. doi: 10.1007/s12583-019-1252-7
Citation: Zhaojun Song, Huimin Liu, Fanxue Meng, Xingyu Yuan, Qiao Feng, Dingwu Zhou, Juan Ramon Vidal Romaní, Hongbo Yan. Zircon U-Pb Ages and Hf Isotopes of Neoproterozoic Me-ta-Igneous Rocks in the Liansandao Area, Northern Sulu Orogen, Eastern China, and the Tectonic Implications. Journal of Earth Science, 2019, 30(6): 1230-1242. doi: 10.1007/s12583-019-1252-7

Zircon U-Pb Ages and Hf Isotopes of Neoproterozoic Me-ta-Igneous Rocks in the Liansandao Area, Northern Sulu Orogen, Eastern China, and the Tectonic Implications

doi: 10.1007/s12583-019-1252-7
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  • Corresponding author: Fanxue Meng
  • Received Date: 27 Jun 2019
  • Accepted Date: 08 Oct 2019
  • Publish Date: 01 Dec 2019
  • The Sulu Orogen preserves the Neoproterozoic tectonic-magmatic events, corresponding to the breaking up of the Rodinia supercontinent. The ages and petrogenesis of meta-igneous rocks in the Liansandao area in the northern Sulu Orogen are not well-constrained. This study reports zircon U-Pb ages and Hf isotopes of these rocks from the Liansandao area. Three meta-igneous rock samples give similar weighted mean 206Pb/238U ages of 744±11, 767±12, and 762±15 Ma, respectively, indicating the Neoproterozoic crystallization ages. These rocks formed coevally with the Wulian and Yangkou intrusions that located along the Yantai-Qingdao-Wulian fault zone. The Neoproterozoic ages indicate that the meta-igneous rocks from the Liansandao area have affinity to the Yangtze Block. The three samples have εHf(t) values of -7.2- -10.5, -6.0- -17.5, and -6.8- -12.0, respectively. These negative εHf(t) values indicate a primarily crustal source. However, the widely various εHf(t) values that are higher than the continental crust, suggesting magma mixing between mantle-derived materials and the continental crust or source heterogeneity. Combined with the Hf model ages and geochemical characteristics, the monzodiorite (sample LSD-2) is most likely to be mantle-derived magma then interacted with ancient continental crust, and the granitic protolith (samples LSD-1 and LSD-3) in the Liansandao area might derive from the re-melting of a Paleoproterozoic continental crust at ~750 Ma, resulting from the upwelling and underplating of mantle-derived magma formed in an extensional setting due to the break- up of the Rodinia supercontinent.


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