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where we used Equation (29).
where we have used Equation 4.3.
For this reason, we used Equation 23.
We used Equation 5 to obtain the combination.
In fact, depending on which kernel is used, Equation 5 could introduce additional errors.
We used Equation 18 to normalize the initial direct-relation IT2 FS matrix.
Hence, we used Chave et al. [65] commonly used equation for tropical moist forests.
We used Equation 8 to compute the reflectivity spectrum for a multilayered dielectric structure.
We used Equation (9) but instead of we used as (10 1010 10
We assigned 0.8 for crossover fraction, and used Equation (24) for reproduction of the elite counts.
The recent volcano seismology literature has used Equation 1 (e.g., Kawakatsu and Yamamoto 2007; Kumagai 2009; Chouet 2013), whereas earlier studies generally used Equation 2 (e.g., Chouet 1996; Julian et al. 1998; Dreger et al. 2000; Nishimura and Iguchi 2011).
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