Titlebook: Schmerztherapie bei Kindern; Boris Zernikow Book 20011st edition Springer-Verlag Berlin Heidelberg 2001 Anamnese.Angst.H?matologie.Impfung

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書目名稱Schmerztherapie bei Kindern影響因子(影響力)




書目名稱Schmerztherapie bei Kindern影響因子(影響力)學(xué)科排名




書目名稱Schmerztherapie bei Kindern網(wǎng)絡(luò)公開度




書目名稱Schmerztherapie bei Kindern網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Schmerztherapie bei Kindern被引頻次




書目名稱Schmerztherapie bei Kindern被引頻次學(xué)科排名




書目名稱Schmerztherapie bei Kindern年度引用




書目名稱Schmerztherapie bei Kindern年度引用學(xué)科排名




書目名稱Schmerztherapie bei Kindern讀者反饋




書目名稱Schmerztherapie bei Kindern讀者反饋學(xué)科排名

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point at beam-column connections was analyzed to determine the damage index and damage level of the building. The building performed the early yielding point at 3.115?s for beam element at intensity 0.20?g. Based on result, the critical frame 2A/F–B of the building can stand an earthquake happen wi

mitral-valve

砍伐

H. Denecke,C. Hünseler rate at less power intensity and less oscillations amplitude at 35?% is statistically significant and higher of bacterial disruption than the greater power intensity, .?=?001. Meanwhile, higher flow rate was affected by increases of cycle treatment and consequences of the higher disruption of . cel

流動性

Aerate

irreparable

B. Jung,S. Würdischnces, model nonlinearities, buoyancy force, hydrodynamic drag force and added mass on the HAUV system are considered as a control scheme performance while the convergence curve of the fitness function indicates the performance of optimization algorithm. Finally, the suggested tuning method promises

細絲

B. Zernikow,G. Bürk,E. Micheldata. Normalized data very beneficial in features extraction process, so that the significant odor-patterns can be established. In this study, geometry average calculation method was applied in order to establish the odor-profile for lubricant oil sample. The odor-pattern then were classified using

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B. Zernikowl crust. One of the most significant achievements of volcano InSAR has been the identification and characterisation of magma inputs into the crust that would have otherwise gone unnoticed (e.g. Lu and Dzurisin .). Such observations of magma movement and other slow, long-term processes are crucial in