Dieser Beitrag bringt einen Vorschlag, die Kurtose nach einer neuen Methode zu berechnen. Die Vorteile dieser Methode werden vom statistischen und geologischen Gesichtspunkt aus kurz besprochen. Vielleicht bietet diese neue Berechnung der Kurtose die Möglichkeit, die Sedimente leichter zu differenzieren.The author show the possibility of computing kurtosis in a manner which parallels Wentworth's computation of skewness. They offer for further consideration various suggestions on the possible statistical and sedimentological advantages of this "new" coefficient. Besides the test or check value, the method permits a greater spread of kurtic value in the central area and in addition would perhaps permit a better differentiation between sedimen...
We reconsider the derivation of Blest’s (2003) skewness adjusted version of the classical moment-bas...
This research is an exposition of D. N. Joanes and C. A. Gill\u27s study on Comparing Measures of Sa...
An increase in kurtosis is achieved through the location- and scale-free movement of probability mas...
Moment measures are widely used to describe the properties of samples. The third and fourth nmments,...
Numerous measures are used in the literature to describe the grain-size distribution of sediments. C...
For symmetric unimodal distributions, positive kurtosis indicates heavy tails and peakedness relativ...
In this paper some new indices of sample shape ( skewness and kurtosis) are defined by means of lett...
The standardized fourth central moment (standardized according to the variance) is often regarded as...
We critically review the development of the concept of kurtosis. We conclude that it is best to defi...
We critically review the development of the concept of kurtosis. We conclude that it is best to defi...
Two families of kurtosis measures are defined as K1(b) = E[ab-|z|] and K2(b) = E[a(1 - |z|b)] where ...
Theoretical considerations of kurtosis, whether of partial orderings of distributions with respect t...
Variations in skewtless and kurtosis in sediments from the central northeastern Irish Sea can '...
A common characteristic of concentration data compilations for geochemical reference materials (GRM)...
Modern depositional environment are mainly investigated in terms of internal sedimentary structures ...
We reconsider the derivation of Blest’s (2003) skewness adjusted version of the classical moment-bas...
This research is an exposition of D. N. Joanes and C. A. Gill\u27s study on Comparing Measures of Sa...
An increase in kurtosis is achieved through the location- and scale-free movement of probability mas...
Moment measures are widely used to describe the properties of samples. The third and fourth nmments,...
Numerous measures are used in the literature to describe the grain-size distribution of sediments. C...
For symmetric unimodal distributions, positive kurtosis indicates heavy tails and peakedness relativ...
In this paper some new indices of sample shape ( skewness and kurtosis) are defined by means of lett...
The standardized fourth central moment (standardized according to the variance) is often regarded as...
We critically review the development of the concept of kurtosis. We conclude that it is best to defi...
We critically review the development of the concept of kurtosis. We conclude that it is best to defi...
Two families of kurtosis measures are defined as K1(b) = E[ab-|z|] and K2(b) = E[a(1 - |z|b)] where ...
Theoretical considerations of kurtosis, whether of partial orderings of distributions with respect t...
Variations in skewtless and kurtosis in sediments from the central northeastern Irish Sea can '...
A common characteristic of concentration data compilations for geochemical reference materials (GRM)...
Modern depositional environment are mainly investigated in terms of internal sedimentary structures ...
We reconsider the derivation of Blest’s (2003) skewness adjusted version of the classical moment-bas...
This research is an exposition of D. N. Joanes and C. A. Gill\u27s study on Comparing Measures of Sa...
An increase in kurtosis is achieved through the location- and scale-free movement of probability mas...