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Page 1163
( iv ) Select randomly a thickness remained in a given state . The distribu- from the frequency distribution of the tions from Posey County are strongly jth lithology . ( v ) Repeat the above negatively skewed , because sedimenta- ...
( iv ) Select randomly a thickness remained in a given state . The distribu- from the frequency distribution of the tions from Posey County are strongly jth lithology . ( v ) Repeat the above negatively skewed , because sedimenta- ...
Page 1287
reduces the observed radio flux from * to S , given by Im at this maximum point is given by the relation S = ( S * / - ) ( 1 - e - ) . ( A - 7 ) em – 1 = mm [ 1 + ( 2a / 5 ) ] . ( A - 13 ) For sufficiently low frequencies the ...
reduces the observed radio flux from * to S , given by Im at this maximum point is given by the relation S = ( S * / - ) ( 1 - e - ) . ( A - 7 ) em – 1 = mm [ 1 + ( 2a / 5 ) ] . ( A - 13 ) For sufficiently low frequencies the ...
Page 1320
( 9 ) . by the electrons at high harmonics of I have examined the question of their gyrofrequency , which is given by negative absorption again , and have found that it is possible after all . This å í ( 1 ) conclusion differs from ...
( 9 ) . by the electrons at high harmonics of I have examined the question of their gyrofrequency , which is given by negative absorption again , and have found that it is possible after all . This å í ( 1 ) conclusion differs from ...
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