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Full text: Die Anwendung geostatistischer Verfahren zur Interpretation von gravimetrischen und magnetischen Felddaten

126 
A = 1 
2) e[ H 2 (r,rj)] = 
/2n a_ 
2r\r — (tj — tj) 2 / 2 o 2 
d tj 
(B-1) 
1 -exp f--a 
T^Y ^1 2 o 2 
-2 (2ro 2 - J ) )r l 
exp 
2o n 
d 71 
Mit 
Gradstein (1981), Gleichung 3.323 Nr. 2 
OO 
2 i—» 
exp (-p 2 x 2 i qx) d x = exp ( 
(B-2) 
folgt: 
e[ H 2 (r ,r]) ] = 
e -2T]r e 2a^r 2 
(Gleich. (3-26)) 
31 E [ D2(r - S) ] - TZTc 
00 
J ( ’ _ e " r)i 
-(8 - 8 ) z / 2 “ 2 
d 8 
= A - B +C 
mit 
A = 
OO 
^°s l 
-(8 - 8 ) 2 / 2 a? 
e 5 d8 
(B-3) 
B = 
■/¿ix" o 
J 
2 1 e" Sr - e 
-(8 -8) 2 /2o| 
dS 
(B-4) 
C = 
OO 
J 
- (8 - 8) 2 / 2 o 2 
e~ 25 r • e 
dS 
(B—5) 
Für Gleichung (B-3) ergibt sich sofort:
	        
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