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    SHRIMP U-Pb zircon geochronology of granulites at Rimana(Southern Tibet)in the central segment of Himalayan Orogen [查看] LIDeweiLIAOQunanYUANYanmingWANYushengLIUDeminZHANGXionghuaYIShunhua1CAOShuzhaoXIEDefan
    Mineralizing age of the Rushan lode gold deposit in the Jiaodong PeninsulaSHRIMP U-Pb dating on hydrothermal zircon [查看] HUFangfangFANHongruiYANGJinhuiWANYushengLIUDunyiZHAIMingguoJINChengwei
    The Dabie Orogen as the early Jurassic sedimentray provenanceConstraints from the detrital zircon SHRIMP U-Pb dating [查看] LIRenweiWANYushengCHENGZhenyuZHOUJianxiongXUYunhuaLIZhongJIANGMaosheng
    The age of the base of the Paleoproterozoic Hutuo Group in the Wutai Mountains area, North China Craton SHRIMP zircon U-Pb dating of basaltic andesite [查看] DULiLinYANGChongHuiGUOJingHuiWANGWeiRENLiuDongWANYuShengGENGYuanSheng
    SHRIMP U-Pb dating for a K-bentonite bed in the Tieling Formation,North China [查看] SUWenBoLIHuaiKunHUFFWDETTENSOHNFRZHANGShiHongZHOUHongYingWANYuSheng
    A SHRIMP U-Pb zircon age of 1437±21 Ma was obtained for a recently discovered K-bentonite bed in the Tieling Formation,situated northeast of Beijing at the boundary between Liaoning and Hebei provinces, on the northern margin of the North China Craton (NCC). The SHRIMP U-Pb age places Tieling Formation near the end of the Calymmian Period of the early Mesoproterozoic Era. In addition, a SHRIMP U-Pb zircon date of 1372±18 Ma was acquired for K-bentonite beds in the overlying,dark-shale-dominated Xiamaling Formation from the same location northeast of Beijing. This date assigns a similar Mid-Mesoproterozoic (Ectasian Period) age for the Xiamaling Formation, as have previously determined dates from other sections northwest of Beijing. These dates indicate that the Tieling and Xiamaling formations, as well as the related succession in the eastern part of the Yanshan Mountains, represented by the well-known Meso- to Neoproterozoic standard section in Jixian, can be correlated well with sections northwest of Beijing in the western part of the Yanshan Mountains. In other words, the boundary between the Calymmian and Ectasian periods in the northern parts of the NCC is marked by the unconformity between the Tieling and Xiamaling formations in the northern NCC. This boundary was previously ascribed to the “Qinyu Orogeny” and thought to be of Grenville age. In this regard, the conventional “Qinyu Orogeny” should now be regarded as a short-lived regional uplift during Early Mesoproterozoic time, rather than a result from the Grenvillian assembly of the NCC to the Rodinia Supercontinent (~1.0 Ga).
    Report on 3.4 Ga SHRIMP Zircon Age from the Yuntaishan Geopark in Jiaozuo, Henan Province [查看] GAOLinzhiZHAOTingWANYushengZHAOXunMAYinshengYANGShouzheng
    SHRIMP zircon U-Pb dating for subduction-related granitic rocks in the northern part of east Junggar, Xinjiang [查看] ZHANGZhaochongYANShenghaoCHENBailinZHOUGangHEYongkangCHAIFengmeiHELixinWANYusheng
    Polyphase tectonothermal history recorded in granulitized gneisses from the North Qaidam HPUHP metamorphic terrane,Western Chinaevidence from zircon U-Pb geochronology [查看] ZhangJianxinChristopherG.MattinsonMengFancongWanYushengDongkuoan
    Finding of Neoproterozoic (~775 Ma) magmatism recorded in metamorphic complexes from the North Qilian orogen Evidence from SHRIMP zircon U-Pb dating [查看] Chien-YuanTsengHoung-YiYangWANYushengLIUDunyiDa-JenWenTzung-ChiLinKuo-AnTung
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