Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
the pertinent kernels and their form for two particularly simple structures. Note that in the case of a vanishing conductor (i.e. in the examples h -> m, or k + 0) the kerne1.s K- and M have to agree with the kernels of (5.8a) and (5.8~1, respectively. Tile function L occurring in the P-kernel of the uniform half-space 2' model is the modified Struve function of the second order (cf. Abramowitz and Stegun, p. 498).
- Page 15 and 16: with " the abbreviation + - 1 - ? =
- Page 17 and 18: 2n -i~cr cos (8-$1 -iKrcU J e ~B=J
- Page 19 and 20: In the 1irnl.t a -+ o, I +- m, M =
- Page 21 and 22: -- 2.5. Definition -- of the transf
- Page 23 and 24: we arrive at - v The same appl-ies
- Page 25 and 26: ) Computation of ---- C for a laxez
- Page 27 and 28: The approximate interpretation of C
- Page 29 and 30: I ~ispersi-on relations I Dispersio
- Page 31 and 32: where L is a positively oriented cl
- Page 33 and 34: 1 2 3 4 CPD 1 2 3 4 CPD - g) Depend
- Page 35 and 36: The TE-mode has no vertical electri
- Page 37 and 38: i I Earth Anomalous domain 3.2. Air
- Page 39 and 40: Hence, the conductivity is to be av
- Page 41 and 42: The RHS i.s a closed line integral
- Page 43 and 44: 4. Having determined B;, the coeffi
- Page 45 and 46: 3.4. Anomalous region as basic doma
- Page 47 and 48: - 6 and 6= can be so adjusted that
- Page 49 and 50: From the generalized Green's theore
- Page 51 and 52: and y can again be so adjusted that
- Page 53 and 54: 4.2. In3ral - --- equation method L
- Page 55 and 56: The element GZx is needed for all z
- Page 57 and 58: With this knowledge of the behaviou
- Page 59 and 60: After having determined Qzr VJ,; @,
- Page 61 and 62: 4.3. The surface inteyral approach
- Page 63 and 64: F At the vertical boundaries the co
- Page 65: The four equations A A A A H = i sg
- Page 69 and 70: 6.1.2. The llnear inverse problem T
- Page 71 and 72: should be small. Hence it required
- Page 73 and 74: are proportional to the long axes o
- Page 75 and 76: Suppose that an approximation & to
- Page 77 and 78: - Only for P M, _A - is the M compo
- Page 79 and 80: Now m Division by f !, (0) :f; (0)
- Page 81 and 82: 6.4. Quasi-linearization - of the o
- Page 83 and 84: Introducing the new transfer functi
- Page 85 and 86: 'periments are done with profiles o
- Page 87 and 88: The vertical magngtic component HZ
- Page 89 and 90: the surface. Only near certai-n sul
- Page 91 and 92: Since CI and CII cannot be zero for
- Page 93 and 94: Suppose the lateral variations u ar
- Page 95 and 96: , , The formula for E applies also
- Page 97 and 98: h melting occurs, the conduction th
- Page 99 and 100: 9 (solar quiet) varia-tions: On the
- Page 101 and 102: polar substorlns is j.n mid-latitud
- Page 103 and 104: Overall - depth - distribution -. D
- Page 105 and 106: The next diagram shows the resultin
- Page 107 and 108: 8.2 Or~anisation and objectives -.
- Page 109 and 110: Tests for the assumption of a layer
- Page 111 and 112: The in-phase induction arrow is def
- Page 113 and 114: If, for instance E = V and H = U, t
- Page 115 and 116: . . These sets of tPansfe$fUnCtions
the pertinent kernels and their form for two particularly simple<br />
structures. Note that in the case of a vanishing conductor (i.e.<br />
in the examples h -> m, or k + 0) the kerne1.s K- and M have to<br />
agree with the kernels of (5.8a) and (5.8~1, respectively. Tile<br />
function L occurring in the P-kernel of the uniform half-space<br />
2'<br />
model is the modified Struve function of the second order (cf.<br />
Abramowitz and Stegun, p. 498).
Change language