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| 1 | Late Cenozoic deformation subsequence in northeastern margin of Tibet --Detrital AFT records from Linxia Basin显示文摘Two events of Tibet uplifting are revealed by detrital apatite fission track (AFT) age data from Linxia Basin. They occurred at about 14 and 5.4-8.0 MaBP respectively. We interpret the first one to be related to the uplifting of the northern Tibet, which might have resulted from convectively removing the thickened lower lithosphere. The second one is a result of Laji Mountain uplifting. Numerous studies of the Tibetan Plateau suggest that the onset time of the deformation in the northeastern margin of Tibetan Plateau and the time of Tibet attaining to its present elevation is about 8 MaBP. They are approximately coincident with the uplift of Lajishan Mountain. It suggests that the northeastern margin of Tibet propagated northeastwardly to its present site in about 8 MaBP for accommodating the sustained convergence between India-Eurasia plate and for keeping its high elevation. The active block pattern dominating the strong earthquake distribution of Chinese continent probably formed at about 8.0-5.4 MaBP. | ZHENG Dewen (郑德文) ZHANG Peizhen (张培震) WAN Jinglin (万景林) LI Chuanyou (李传友) CAO Jixiu (曹继秀) | 2003 | Science China Earth Sciences2003，46，z2： | 25 |
| 2 | Fission track dating of the Cenozoic uplift in Mabian area, southern Sichuan Province, China显示文摘The apparent ages of samples are obtained from fission track dating of apatite samples collected from the fault zones in Mabian area, southern Sichuan Province. In addition, thermal history is simulated from the obtained data by applying AFT Solve Program, to acquire the thermal evolution history of the samples. The result shows that tectonically the Mabian area was relatively stable between 25 and 3 Ma, compared to the inner parts and other marginal areas of the Tibetan Plateau. The studied area had little response to the rapid uplift events that occurred for several times in the Tibetan Plateau during 25-3 Ma. The latest thermal event related to the activity of the Lidian fault zone (about 8 Ma ) is later than that of the Ebian fault zone (18-15 Ma ) to the west, indicating to some extent that the evolution of fault activity in the Mabian area has migrated from west to east. The latest extensive tectonic uplift occurred since about 3 Ma. As compared with the Xianshuihe fault zone, the Mabian area is closer to the east- ern margin of the plateau, while the time of fast cooling event in this area is later than that in the southeast segment of the Xianshuihe fault zone (3.6-3.46 Ma ). It appears to support the assumption of episodic uplift and stepwise outward extension of the eastern boundary of the Tibetan Plateau in late Cenozoic. | AN YanFen HAN ZhuJun WAN JingLin | 2008 | Science China Earth Sciences2008，51，9： | 14 |
| 3 | Geological analysis and FT dating of the large-scale right-lateral strike-slip movement of the Red River fault zone显示文摘Tectonically, the large-scale right-lateral strike-slip movement along the Red River fault zone is char-acterized at its late phase with the southeastward extension and deformation of the Northwestern Yunnan normal fault depression on its northern segment, and the dextral shear displacement on its central-southern segment. Research of the relations between stratum deformation and fault movement on the typical fault segments, such as Jianchuan, southeast Midu, Yuanjiang River, Yuanyang, etc. since the Miocene Epoch shows that there are two times dextral faulting dominated by normal shearing occurring along the Red River fault zone since the Miocene Epoch. The fission track dating (abbrevi-ated to FT dating, the same below) is conducted on apatite samples collected from the above fault segments and relating to these movements. Based on the measured single grain’s age and the con-fined track length, we choose the Laslet annealing model to retrieve the thermal history of the samples, and the results show that the fault zone experienced two times obvious shear displacement, one in 5.5 ± 1.5 MaBP and the other in 2.1± 0.8 MaBP. The central-southern segment sees two intensive uplifts of mountain mass in the Yuanjiang River-Yuanyang region at 3.6―3.8 MaBP and 1.6―2.3 MaBP, which correspond to the above-mentioned two dextral normal displacement events since the late Miocene Epoch. | XIANG HongFa WAN JingLin HAN ZhuJun GUO ShunMin ZHANG WanXia CHEN LiChun DONG XingQuan | 2007 | Science China Earth Sciences2007，50，3： | 10 |
| 4 | Late Mesozoic Thermotectonic Evolution of the Jueluotage Range,Eastern Xinjiang,Northwest China:Evidence from Apatite Fission Track Data显示文摘摘要:尽管许多作者强调了变丑的新生代历史,发掘并且在与印度亚洲碰撞有关的 Tianshan 区域冷却,几乎不对压缩的中生代历史被知道并且在 Tianshan 以内高举。以便关于中生代发掘历史和在东方 Tianshan 冷却的进程获得信息,磷灰石上的分裂磁道方法被使用。采样在 Jueluotage 范围被做。三件样品(Z001-Z003 ) 在 Yandong pluton 的地上凿穿 ZK6301 从花岗石被拿;从比是的 pluton 年龄年轻得多的 97.0 ~ 87.6 妈的年龄范围在 334 点由 U-Pb 锆石标明日期 ????????? Y ?? 霈吗?? | ZHU Wenbin WAN Jinglin SHU Liangshu ZHANG Zhiyong SU Jinbao SUN Yah GUO Jichun ZHANG Xueyun | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 4 |
| 5 | Insufficient thermalization effects on determining fission-track ages显示文摘Fission-Track Dating (FTD) has been developed as a useful technique for geological studies. Parent elements are measured by counting 235 U tracks induced by thermal neutrons. If insufficient thermalization occurs, fission of 238 U and 232 Th will be induced, and further measurement error will be introduced. Therefore, whether the neutrons are well thermalized or not will affect the FTD results. Due to requirement of safe operation, the 101 reactor was terminated in 2007. By using the 492 reactor as the new thermal neutron reactor, our present paper will attempt to study the feasibility and the potential influence on FTD. By irradiating monitor glass SRM612 and CN5 in pairs, we will study the thermalization situation of the 492 reactor. Irradiated data show that thermal neutrons are not evenly distributed either in horizontal or in vertical dimension. Especially, horizontal heterogeneity is obvious. But we discovered that proper irradiation position in the reactor can meet the requirement of FTD. Under the current irradiation condition, we calculated and assessed the insufficient thermalization effects on determining fission-track ages. We found that the difference between the 232 Th/ 238 U ratios of samples and standards is the main factor to the experiment results. The results will not be affected if the 232 Th/ 238 U value of samples is equal to the standard samples. However, if the 232 Th/ 238 U ratio is larger than that of the standards, the results will be smaller than actual ages. Comparatively, the ages will be more than expected if the 232 Th/ 238 U ratio is less. Therefore, to reduce the irradiation error, we suggest either locating the position of irradiation strictly, or minimizing the influence of lateral heterogeneity by reducing the amount of each sample package. Additionally, accuracy of the experimental results can be improved by increasing standard samples to adjust ζ value and using the monitor of standard glass SRM612 and CN5 together. | PANG JianZhang ZHENG DeWen WAN JingLin LI DaMing ZHANG PeiZhen YANG Jing | 2013 | Science China Earth Sciences2013，56，7： | 2 |
| 6 | Combined apatite fission-track dating, chlorine and REE content analysis by LA-ICPMS显示文摘As one of the best established low temperature thermochronology techniques,apatite fission-track(AFT)analysis has proved an important tool for constraining a wide variety of upper crustal processes,e.g.,landscape evolution,hydrocarbon exploration and tectonics[1].The most common method employed for AFT analysis is the external detector method(EDM)[1]and this involves the thermal neutron irradiation of samples for determination of | Jianzhang Pang Dewen Zheng Yan Ma Ying Wang Ying Wu Jinglin wan Jingxing Yu Youjuan Li Yizhou Wang | 2017 | Science Bulletin2017，62，22： | 2 |
| 7 | Late Cenozoic geological evolu- tion of the foreland basin bordering the West Kunlun range in Pulu area: Constraints on timing of uplift of no,hem margin of the Ti- betan Plateau显示文摘 | Wang Erchie Wan Jinglin Liu Jiaqi | 2003 | Journal of Geophysical Research2003，108，8： | 1 |
| 8 | The sequence of tectonic deformation since Late Cenozoic of northeastern margin of Qinghai-Tibet Plateau显示文摘 | Zheng Dewen Zhang Peizhen Wan Jinglin | 2003 | Science in China2003，，： | 1 |
| 9 | Late Cenozoic geological evolution of the foreland basin bordering the West Kunlun range in Pulu area: Constraints on timing of uplift of northern margin of the Tibetan Plateau显示文摘 | Erchie Wang Jinglin Wan Jiaqi Liu | 2003 | Journal of Geophysical Research2003，108，138： | 1 |
| 10 | Late Cenozoic geological evolution of the foreland basin bordering the West Kunlun range in Pulu area:Constraints on timing of uplift of northern margin of the Tibetan Plateau 显示文摘 | Erchie Wang Jinglin Wan Jiaqi Liu et el | 2003 | Journal of Geophysical Research2003，1088，： | 1 |
| 11 | Cenozoic Exhumation of Larsemann Hills,East Antarctica:Evidence from Apatite Fission-track Thermochronology显示文摘新生代发掘发生在 Larsemann 山,东方南极洲吗?在现在的纸,我们越过东方南极洲的 Larsemann 山进行了磷灰石分裂轨道 thermochronologic 研究。我们的工作在 49.8 点揭示一个新生代发掘事件 ? 跱?????? | CHEN Xuanhua JIANG Rongbao WAN Jinglin XU Gang JIANG Mei CHEN Danhong | 2010 | Acta Geologica Sinica(English Edition)2010，84，2： | 1 |
| 12 | Microwave shock motivating the Sr substitution of 2D porous GdFeO_(3) perovskite for highly active oxygen evolution显示文摘The incorporation of partial A-site substitution in perovskite oxides represents a promising strategy for precisely controlling the electronic configuration and enhancing its intrinsic catalytic activity.Conventional methods for A-site substitution typically involve prolonged high-temperature processes.While these processes promote the development of unique nanostructures with highly exposed active sites,they often result in the uncontrolled configuration of introduced elements.Herein,we present a novel approach for synthesizing two-dimensional(2D)porous GdFeO_(3) perovskite with A-site strontium(Sr)substitution utilizing microwave shock method.This technique enables precise control of the Sr content and simultaneous construction of 2D porous structures in one step,capitalizing on the advantages of rapid heating and cooling(temperature~1100 K,rate~70 K s^(-1)).The active sites of this oxygen-rich defect structure can be clearly revealed through the simulation of the electronic configuration and the comprehensive analysis of the crystal structure.For electrocatalytic oxygen evolution reaction application,the synthesized 2D porous Gd_(0.8)Sr_(0.2)FeO_(3) electrocatalyst exhibits an exceptional overpotential of 294 mV at a current density of 10 mA cm^(-2)and a small Tafel slope of 55.85 mV dec^(-1)in alkaline electrolytes.This study offers a fresh perspective on designing crystal configurations and the construction of nanostructures in perovskite. | Jinglin Xian Huiyu Jiang Zhiao Wu Huimin Yu Kaisi Liu Miao Fan Rong Hu Guangyu Fang Liyun Wei Jingyan Cai Weilin Xu Huanyu Jin Jun Wan | 2024 | Journal of Energy Chemistry2024，88，1： | 0 |
| 13 | Microwave-assisted exploration of the electron configuration-dependent electrocatalytic urea oxidation activity of 2D porous NiCo_(2)O_(4)spinel显示文摘Urea holds promise as an alternative water-oxidation substrate in electrolytic cells.High-valence nickelbased spinel,especially after heteroatom doping,excels in urea oxidation reactions(UOR).However,traditional spinel synthesis methods with prolonged high-temperature reactions lack kinetic precision,hindering the balance between controlled doping and highly active two-dimensional(2D)porous structures design.This significantly impedes the identification of electron configuration-dependent active sites in doped 2D nickel-based spinels.Herein,we present a microwave shock method for the preparation of 2D porous NiCo_(2)O_(4)spinel.Utilizing the transient on-off property of microwave pulses for precise heteroatom doping and 2D porous structural design,non-metal doping(boron,phosphorus,and sulfur)with distinct extranuclear electron disparities serves as straightforward examples for investigation.Precise tuning of lattice parameter reveals the impact of covalent bond strength on NiCo_(2)O_(4)structural stability.The introduced defect levels induce unpaired d-electrons in transition metals,enhancing the adsorption of electron-donating amino groups in urea molecules.Simultaneously,Bode plots confirm the impact mechanism of rapid electron migration caused by reduced band gaps on UOR activity.The prepared phosphorus-doped 2D porous NiCo_(2)O_(4),with optimal electron configuration control,outperforms most reported spinels.This controlled modification strategy advances understanding theoretical structure-activity mechanisms of high-performance 2D spinels in UOR. | Jun Wan Zhiao Wu Guangyu Fang Jinglin Xian Jiao Dai Jiayue Guo Qingxiang Li Yongfei You Kaisi Liu Huimin Yu Weilin Xu Huiyu Jiang Minggui Xia Huanyu Jin | 2024 | Journal of Energy Chemistry2024，91，4： | 0 |
| 14 | Application of microneedle-based vaccines in biosecurity显示文摘Countries must have strong early warning,detection,and response capabilities in the face of the risks and challenges posed by major infectious diseases and bioterrorism threats.Vaccination is one of the most effective means for countries to maintain biosecurity and respond to bioterrorism attacks.Microneedles are emerging as a potential vaccine delivery method with minimal pain,no bleeding,and the ability to be self-administered,doing away with the need for professional health care workers.This last advantage,particularly if combined with room temperature preservation,could have an important role in improving national biosecurity through large-scale,rapid deployment of a biological vaccine.In this review,we summarized the research status of microneedles,including the types,materials,and production technologies of microneedles.Recent progress regarding microneedles in the field of biosecurity is introduced and challenges in its future application are discussed. | Zhiying Jin Baohua Zhao Wei Wan Yue Li Xuexin Bai Chenyi Hu Jing Wang Yanwei Li Wenwen Xin Lin Kang Hao Yang Jinglin Wang Shan Gao | 2022 | Journal of Biosafety and Biosecurity2022，4，1： | 0 |
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