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| 1 | SHRIMP U-Pb dating for a K-bentonite bed in the Tieling Formation,North China显示文摘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). | SU WenBo LI HuaiKun HUFF W D ETTENSOHN F R ZHANG ShiHong ZHOU HongYing WAN YuSheng | 2010 | Chinese Science Bulletin2010，55，29： | 30 |
| 2 | U-Pb zircon age and Hf isotope compositions of Mesoproterozoic sedimentary strata on the western margin of the Yangtze massif显示文摘Yangtze 山岳的西方的边缘上的 Mesoproterozoic 沉积阶层是一个碎屑状碳酸盐的岩石协会与凝灰岩和暗岩的小数量设置了并且在相对稳定的环境扔了。他们在不同区域分别地作为 Kunyang 组, Huili 组,和 Dongchuan 组被称为。我们执行了从这些组凝灰岩标明日期的锆石 U-Pb。结果,从 Kunyang 组和 Dongchuan 组结合了碎屑状的岩石的由岩屑形成的锆石 U-Pb 年龄,显示沉积从 1050~1000 妈 Kunyang 组和 Huili 组范围变老并且 Kunyang 组和 Huili 组与同时期的 heterotopic 外形属于一个沉积协会。由岩屑形成的锆石年龄和 Hf 同位素作文表明在 Kunyang 组和 Huili 组的碎屑状的材料首先从 Cathaysia 山岳被导出。在 ca.1.5 Ga 和所有锆石的年龄在 Dongchuan 组 clastics 变老的 Dongchuan 组收益的凝灰岩的锆石比 1.5 Ga 旧,显示 Dongchuan 组的沉积发生在迟了的 Mesoproterozoic Changcheng 时期期间。由岩屑形成的锆石的年龄系列显示 Dongchuan 组的碎屑状的材料首先从 Yangtze 山岳的古老的地下室被导出。以上述三个 stratigraphic 单位的锆石的各种各样的类型的一颗系统的 Hf 同位素决心证明在在 1.5 和 1.0 Ga 的锆石的起始的 Hf 价值有快速的举起。Kunyang 组和 Huili 组的沉积特征上的以前的研究证明两个在低岬盆被扔。把我们的数据与以前的研究相结合,我们建议 Kunyang 组和 Huili 组是沉积继任在 Grenvillian 期间在在 Yangtze 山岳和 Cathaysia 山岳之间的合并以后沿着 Yangtze 山岳的南部的方面形成了的低岬盆。Yangtze 山岳和 Cathaysia 山岳的集会从西方逐渐地发展了到东方并且最后在 0.9 Ga 在 Yangtze 山岳的东方片断被完成,代表 Rodinia supercontinent 集会的最后阶段。在锆石的 Hf 同位素作文显示 supercontinent 周期与外壳的生长有一种亲密关系。 | LI HuaiKun ZHANG ChuanLin YAO ChunYan XIANG ZhenQun | 2013 | Science China Earth Sciences2013，56，4： | 23 |
| 3 | Ca. 2.5 Ga TTG rocks in the western Alxa Block and their implications显示文摘The Alxa Block is considered part of the North China Craton, but the unambiguous Archean basement has not been reported. In this study, we present the first evidence of the Neoarchean rocks in the Beidashan area of the western Alxa Block. The petrographic and geochemical data show that these rocks are granodiorite with TTG (tonalite-trondhjemite-granodiorite) characteristics. Zircon U-Pb dating gave an age of 2522±30 Ma for the magmatic core and 2496±11 Ma for the metamorphic recrystallized rim. The near-identical age between the Latest Neoarchean magmatism and the high-grade metamorphism shows that these features were related to the same Latest Neoarchean-Earliest Paleoproterozoic tectonothermal event. The age-corrected Hf (t) value is mainly between 0.4 and 4.9. The two-stage zircon Hf model age ranges from 2.7 to 3.0 Ga, suggesting that the Mesoarchean- Neoarchean (2.7-3.0 Ga) juvenile crust was reworked at the end of the Neoarchean in the western Alxa Block. These data suggest that the western Alxa Block experienced a Mesoarchean-Neoarchean crust growth and Latest Neoarchean-Earliest Paleoproterozoic tectonothermal event similar to the North China Craton. | GONG JiangHua ZHANG JianXin YU ShengYao LI HuaiKun HOU KeJun | 2012 | Chinese Science Bulletin2012，57，31： | 21 |
| 4 | A^2.5 Ga magmatic event at the northern margin of the Yangtze craton:Evidence from U-Pb dating and Hf isotope analysis of zircons from the Douling Complex in the South Qinling orogen显示文摘The poorly studied Douling Complex is a crystalline basement that developed in the Neoproterozoic-Paleozoic weakly metamorphosed to non-metamorphosed strata at the South Qinling tectonic belt.Five banded dioritic-granitic gneiss samples from the Douling Complex were chosen for LA-MC-ICPMS U-Pb zircon dating,which yielded protolith emplacement ages of 2469±22Ma,2479±12 Ma,2497±21 Ma,2501±17 Ma and 2509±14 Ma,respectively.An important peak age of^2.48 Ga was also obtained for a metasedimentary rock in the same region.These discoveries suggest the occurrence of magmatic activity of2.51–2.47 Ga at the northern margin of the Yangtze craton.The age-correctedεHf(t)values obtained from in situ zircon Hf isotopic analysis are mainly between 5.5 and+0.3,and the two-stage zircon Hf model ages range from 3.30 to 2.95 Ga.Considering two important periods of^3.3–3.2 Ga and^2.95–2.90 Ga for the continental crustal growth in the Yangtze craton,we infer that the dioritic-granitic gneisses from the Douling Complex are the products of reworking of Paleo-to Mesoarchean crust at the northern margin of the Yangtze craton at^2.5 Ga.In addition,metamorphic ages of 837±8 Ma and 818±10 Ma were obtained for zircon overgrowth rims from a dioritic gneiss and a metasedimentary rock,indicating that the main phase amphibolite facies metamorphism of the Doulng Complex occurred during the Neoproterozoic,although its geological meaning remains ambiguous. | HU Juan LIU XiaoChun CHEN LongYao QU Wei LI HuaiKun GENG JianZhen | 2013 | Chinese Science Bulletin2013，58，28： | 6 |
| 5 | Geological andgeochronological evidence for the Precambrianevolution of the TarimCraton and surrounding continentalfragments显示文摘 | Lu Songnian Li Huaikun Zhang Chuanlin | 2008 | Precamb Res2008，160，12： | 1 |
| 6 | Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments显示文摘 | Songnian Lu Huaikun Li Chuanlin Zhang Guanghua Niu | 2007 | Precambrian Research2007，，1： | 1 |
| 7 | A group of rifring events in the terminal Paleoproterozoic in the North China Craton显示文摘 | Lu Songnian Yang Chunliang Li Huaikun | 2002 | Gondwana Research2002，5，1： | 1 |
| 8 | Constraining the role of the Qinling orogen in the assembly and break-up of Rodin- ia: Tectonic implications for Neoproterozoic granite occurrences 显示文摘 | Chen Zhihong Lu Songnian Li Huaikun | 2006 | Journal of Asian Earth Sciences2006，，28： | 1 |
| 9 | SHRIMP U–Pb ages of K-bentonite beds in the Xiamaling Formation: Implications for revised subdivision of the Meso- to Neoproterozoic history of the North China Craton显示文摘 | Wenbo Su Shihong Zhang Warren D. Huff Huaikun Li Frank R. Ettensohn Xiaoyu Chen Hongmei Yang Yigui Han Biao Song M. Santosh | 2008 | Gondwana Research2008，，3： | 1 |
| 10 | Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments显示文摘 | Lu Songnian Li Huaikun Zhang Chuanlin | 2008 | Pre- cambrian Research2008，160，1： | 1 |
| 11 | A group of rifting events in the terminal Paleoproterozoic in the North China Craton显示文摘 | LU Songnian YANG Chunliang LI Huaikun | 2002 | Gondwana Research2002，5，1： | 1 |
| 12 | Discovery and Significance of Eclogite-Granitoid Belts in Northwest China显示文摘 | Lu Songnian Zhao Fengqing Mei Hualin Yu Haifeng Li Huaikun Zheng Jiankang | 1999 | Gondwana Research1999，，1： | 1 |
| 13 | Magic hybrid structure as multifunctional electrocatalyst surpassing benchmark Pt/C enables practical hydrazine fuel cell integrated with energy-saving H_(2)production显示文摘A hybrid catalyst structure can provide abundant active sites and tailored electronic properties,but the major challenge lies in achieving delicate control over its composition and architecture to improve the catalytic activity toward different electrochemical reactions simultaneously.Herein,we present the rational design of a magic hybrid structure with low Pt loading(5.90 wt%),composed of CoPt_(3)and CoPt nanoparticles supported on N-doped carbon(CoPt_(3)/CoPt⊂PLNC).Importantly,it shows superior multifunctional catalytic activity in alkaline conditions,requiring a low overpotential of 341 and 20 mV to achieve 10 mA cm^(−2)for the hydrazine oxidation reaction(HzOR)/hydrogen evolution reaction(HER),respectively,and it delivers a half-wave potential of 0.847 V for the oxygen reduction reaction(ORR).Theoretical calculations reveal that the metal-carbon hybrid modulates kinetic behavior and induces electron redistribution,achieving the energetic requirements for multiple electrocatalysis.We demonstrate sustainable H_(2)production utilizing solely the CoPt_(3)/CoPt⊂PLNC catalyst,without external electric power input,suggesting its inspiring practical utility. | Ziyun Li Wentao Wang Qizhu Qian Yin Zhu Yafei Feng Yangyang Zhang Huaikun Zhang Mingyu Cheng Genqiang Zhang | 2022 | eScience2022，2，4： | 0 |
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