Titlebook: Komplexbildung in Lösung; Methoden zur Bestimm Hans L. Schläfer Book 1961 Springer-Verlag oHG. Berlin · Göttingen · Heidelberg 1961 Bindung

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书目名称Komplexbildung in Lösung影响因子(影响力)




书目名称Komplexbildung in Lösung影响因子(影响力)学科排名




书目名称Komplexbildung in Lösung网络公开度




书目名称Komplexbildung in Lösung网络公开度学科排名




书目名称Komplexbildung in Lösung被引频次




书目名称Komplexbildung in Lösung被引频次学科排名




书目名称Komplexbildung in Lösung年度引用




书目名称Komplexbildung in Lösung年度引用学科排名




书目名称Komplexbildung in Lösung读者反馈




书目名称Komplexbildung in Lösung读者反馈学科排名

Pituitary-Gland

Hans L. SchläferKMSS04 satellite altimetry-derived mean sea surface for comparison. This region is of particular interest because of strong crustal movements due to intense tectonic activity that create significant local geoid variations. In this paper, we report on the results of separate SSH surveys that were con

Orgasm

Hans L. SchläferEuropean Space Agency (ESA) as the first of two core missions of ESA’s Earth Explorer Programme to be launched in 2004. The main objective of the GOCE mission is to provide a high-accuracy high-resolution global model of the Earth’s static gravity field and the geoid from a combination of spaceborne

Firefly

Hans L. Schläferced time series of gravity field information to investigate for example ice melting, changes in water storage or the effects of heavy earthquakes. Today the only measurement system which can provide these gravity field solutions without any constraints is the satellite mission GRACE (Gravity Recover

Lumbar-Stenosis

头脑冷静

Hans L. Schläfer undulations. Global gravity field model computed geoid undulations are compared with different sets of GPS/leveling-derived geoid undulations for different spherical harmonic degree expansions. High frequency components of the geoid undulations are estimated from EGM2008 and are removed from the GP

TOM

Hans L. Schläferontrol network—POGK97 (in Polish). Proceedings of the Institute of Geodesy and Cartography, 1999); Sas-Uhrynowski et al. (A new gravimetric control network for Poland. Reports on Geodesy, 2000)) according to the international standards (Boedecker (BGI Bull d’Inf 63:51–56, 1988)). It is based on 12 a

动作谜

Hans L. Schläfert the Esashi Gravity Station (EGS), Iwate Prefecture, Japan. The AGRVP can measure absolute gravity values every 15 minutes with a standard deviation of about 2 × 10.ms. (20.Gals). We compared mean values of more than 400 data obtained by AGRVP at EGS for different periods from July 1994 and found t

羽饰

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Hans L. Schläfera, 1983). The assumed boundary is located from Fossa Magna along the Toyama Trough, Sado Ridge, Okushiri Ridge towards the western egde of Okhotsk Sea (Fig.1). Some features of subducting slab, that is, thrust faulting, are observed by seismic profiling survey in several places along the line, (Naka