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Titlebook: Beginning PhoneGap; Mobile Web Framework Rohit Ghatol,Yogesh Patel Book 2012 Rohit Ghatol and Yogesh Patel 2012

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發(fā)表于 2025-3-26 22:36:39 | 只看該作者
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發(fā)表于 2025-3-27 04:39:50 | 只看該作者
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發(fā)表于 2025-3-27 11:30:16 | 只看該作者
Kinematic and Dynamic Determination of Trajectories for Low Earth Satellites Using GPSchnique gains increasing attention. Different from other approaches for generating kinematic satellite trajectories based on zero- or double-differenced GPS observations the procedure developed at our institute uses zero-differences with differences from epoch to epoch for the phase observable. The
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發(fā)表于 2025-3-27 14:57:53 | 只看該作者
Low-Cost Peptide Microarrays for Mapping Continuous Antibody Epitopes,dy development. Peptide scanning assays enable mapping of continuous epitopes in order to delineate antibody–antigen interactions beyond traditional immunoassay formats. We have developed a relatively low-cost method to generate peptide microarray slides for antibody binding studies that allow for i
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發(fā)表于 2025-3-27 18:42:41 | 只看該作者
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發(fā)表于 2025-3-28 00:35:53 | 只看該作者
Book 2024ors in an increasingly globalized yet unequal world, with a focus on social justice in language education. The chapters offer critical and innovative pedagogical insights that contribute to re-envisioning language and literacy education in the 21.st.?century in a number of educational contexts, incl
38#
發(fā)表于 2025-3-28 04:14:03 | 只看該作者
Cauchy Integrals near ends of the Line of Integrationins arcs. The results obtained below also find application in the more general case in which the density has discontinuities at several points on the line of integration. In this case the path of integration may be split up into separate arcs with the points of discontinuity as ends.
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發(fā)表于 2025-3-28 09:10:08 | 只看該作者
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發(fā)表于 2025-3-28 14:16:46 | 只看該作者
Second- and Third-Order Derivatives of the Somigliana-Pizzetti Reference Gravity Fieldo 10,000?m in altitude differ from an oblate ellipsoid of revolution by less than 0.04?m. It is also shown that this fact can be utilised to approximate the reference gravity gradients through simple formulas.
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