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| 1 | Bayesian sampling plans for exponential distribution based on uniform random censored data 显示文摘 | HUANG Wentao LIN Yupin | 2004 | Computation Statistics & Data Anal- ysis2004，44，4： | 1 |
| 2 | Multivariate analysis of soil heavy metal pollution and landscape pattern in Changhua county in Taiwan 显示文摘 | LIN Yupin TENG Tungpo CHANG Tsunkuo | 2002 | Landscape and Urban Planning2002，62，： | 1 |
| 3 | Developing and comparing optimal and empirical land-use models for the development of an urbanized watershed forest in Taiwan 显示文摘 | LIN Yupin VERBURG P H CHANG Chiru | 2009 | Landscape and Urban Planning2009，92，4： | 1 |
| 4 | Geostatistical Approaches and Optimal Additional Sampling Schemes for Spatial Patterns and Future Sampling of Bird Diversity 显示文摘 | LIN Yupin YEH Mingsheng DENG Dongpo | 2008 | Global Ecology and Biogeography2008，17，： | 1 |
| 5 | Research on the arc type aerostatie bearing for a PCB drilling station显示文摘 | CHEN Mingfei CHEN Yupin LIN Chende | 2002 | Tribology International2002，35，4： | 1 |
| 6 | An improved Bayesian sampling plan for exponential population with type I censoring显示文摘 | Huang Wentao Lin Yupin | 2002 | Communic- tions in Statistics Theory and Methods2002，31，11： | 1 |
| 7 | The genetic relationship between Habo alkaline intrusion and its surrounding deposits, Yunnan Province, China: geological and S–Pb isotopic evidences显示文摘The Habo alkaline intrusion, which is located in the south of the Sanjiang area, Yunnan Province, China, is a typical Cenozoic alkaline intrusion. There are a series of small to medium-sized Au and Pb–(Zn) deposits around this intrusion. Those deposits are spatially associated with the Habo alkaline intrusion.(1) The d^(34) S values of sulfides from Au deposits range from-1.91 % to 2.69 %, which are similar to those of Pb–(Zn) deposits(-3.82 % to-0.05 %) and both indicate a much greater contribution from magma.(2) The Habo alkaline intrusion has relatively homogeneous Pb isotopic compositions with^(206)Pb/^(204) Pb ranging from 18.608 to 18.761,^(207)Pb/^(204) Pb from 15.572 to15.722 and^(208)Pb/^(204) Pb from 38.599 to 39.110. These Pb isotope ratios are similar to those of Au deposits, whose^(206)Pb/^(204) Pb range from 18.564 to 18.734,^(207)Pb/^(204) Pb from15.582 to 15.738 and^(208)Pb/^(204) Pb from 38.592 to 39.319.Pb ratios in both the intrusion and Au deposits suggest that Pb mainly derived from the depth, probably represents a mixture of mantle and crust. Pb–(Zn) deposits, however,show a decentralized trait, and most of them are similar to that of the alkaline intrusion with^(206)Pb/^(204) Pb ranging from18.523 to 18.648,^(207)Pb/^(204) Pb from 15.599 to 15.802, and^(208)Pb/^(204) Pb from 38.659 to 39.206.(3) In the plumbotectonic diagram^(207)Pb/^(204) Pb versus^(206)Pb/^(204) Pb, almost all of Au and Pb–(Zn) deposits have the same projection area with the Habo alkaline intrusion, which indicates that thosedeposits almost share the same source with the alkaline intrusion.(4) Isotopic age of the Habo alkaline intrusion is36–33 Ma, which is similar to that of Beiya, whose orerelated alkaline porphyries age is 38–31 Ma and molybdenite Re–Os age is 36.9 Ma. Therefore, along with S–Pb isotope traits, we suggest that the Habo Au and Pb–(Zn)deposits should be typically Ailaoshan-Red River Cenozoicalkaline-related deposits and ore-forming ages of these deposits should be later than that of the Habo alkaline intrusion. | Zhongneng Meng Qian Zhang Lin Ye Yupin Liu Jiangbo Lan Dapeng Wang | 2016 | Acta Geochimica2016，35，4： | 1 |
| 8 | Improved strap-down coning algorithms显示文摘 | Jiang Yeon Fuh Lin Yupin | 1992 | IEEE Transaction on Aerospace and Electronic Systems1992，28，2： | 1 |
| 9 | Detecting the landcover changes induced by large-physical disturbances using landscape metrics, spatial sampling, simulation and spatial analysis显示文摘 | CHU Hongjay LIN Yupin HUANG Yulong | 2009 | Sensors2009，9，9： | 1 |
| 10 | Structural analysis of a nanoparticle containing a lipid bilayer used for detergent-free extraction of membrane proteins显示文摘在过去几年里,在为稳定包含嵌入的蛋白质的类脂化合物膜的 nanoparticles 的使用有生长。这些 bionanoparticles 由维持类脂化合物 bilayer 必需品到蛋白质完整和活动提供一个解决方案给膜蛋白质隔离的挑战性的问题。我们以前描述了 amphipathic 聚合物的使用(poly (styrene-co-maleic 酸) , SMA ) 与包含嵌入的蛋白质的一个类脂化合物 bilayer 核心生产 discoidal nanoparticles。然而, nanoparticle 本身的结构还没是坚定的。这在理解 SMA 怎么稳定包含的 bilayer 并且 bilayer 怎么身体上联系和在结构上到 unencapsulated 类脂化合物 bilayer 离开主要差距。在这份报纸,我们由描述从小角度中子散布使用数据的 SMA 类脂化合物粒子( SMALP )(圣)的结构处理这个问题,电子显微镜学(他们),稀释全部的思考 Fourier 变换红外线的光谱学( ATR-FTIR ),微分扫描热量测定( DSC )和原子磁性的回声光谱学( NMR )。我们证明粒子是塑造的圆盘包含环绕的一只聚合物手镯类脂化合物 bilayer。在 bilayer 和聚合物以内的单个部件的结构和取向是坚定的证明在 SMA 以内的苯乙烯一半在类脂化合物酰链之间设置。包含的 bilayer 的尺寸也被决定并且匹配为自然的膜测量的那些。一起拿,对 SMALP 的结构的描述在膜蛋白质生产和分析为未来开发和 SMALP 的应用形成基础。 | Mohammed Jamshad Vinciane Grimard Ilaria Idini Tim J. Knowles Miriam R. Dowle Naomi Schofield Pooja Sridhart Yupin Lin Rachael Finka Mark Wheatley Owen R. T. Thomas Richard E. Palmerr Michael Overduin Cedric Govaerts Jean-Marie Ruysschaert Karen J. Edler Tim R. Dafforn | 2015 | Nano Research2015，8，3： | 0 |
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