Titlebook: Geomathematics: Theoretical Foundations, Applications and Future Developments; Frits Agterberg Book 2014 Springer International Publishing

異國(guó)

書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments影響因子(影響力)




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments影響因子(影響力)學(xué)科排名




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments網(wǎng)絡(luò)公開度




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments被引頻次




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments被引頻次學(xué)科排名




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments年度引用




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments年度引用學(xué)科排名




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments讀者反饋




書目名稱Geomathematics: Theoretical Foundations, Applications and Future Developments讀者反饋學(xué)科排名

Biomarker

逢迎春日

dagger

https://doi.org/10.1007/978-3-658-34563-1l’s equation (.. Agterberg 1974) for linear relationship between two variables that are both subject to error can be regarded as a special case of MLFR..Multiple regression can be used for curve-fitting if the relationship between two variables is not linear but other explanatory variables have to b

表主動(dòng)

emulsify

https://doi.org/10.1007/978-3-658-25298-4ntly used geostatistical semivariograms including the spherical and exponential models allow for a nugget effect at their origin representing non-zero variance and assume asymptotic convergence to a constant value representing regional variance at large sampling intervals exceeding a range. However,

emulsify

Wolf J. Schünemann,Stefan Steigerf the first computer-based methods widely applied in geophysics, stratigraphy and physical geography in the 1960s. Initially, it was assumed that the residuals from a best-fitting trend surface should be independent and normally distributed but Watson (J Int Assoc Math Geol 3:215–226, 1971) clarifie

admission

使尷尬

https://doi.org/10.1007/978-3-662-67914-2this chapter. Initially, ranking is illustrated by application to a simple, artificial dataset. Scaling is explained as a refinement of ranking. Implications of techniques of sampling stratigraphic sections are discussed. RASC probable positions with error bars can be determined in different section

偽造者