Corelogger Protocol

where core is the diamagnetic core component, P and L are the Pauli and Landau-Peierls spin sus- ceptibilities of conduction electrons, and VV indi- cates the orbital contribution

Since each polarizer acts only as a polarization-sensitive filter to transmit the field com- ponent of a particular polarization, the phenomenon described in (b) may not seem

We see now, the transmission is a function of θ and the maximum transmission occurs at θ = 45 ◦ , as well as losing 50 % in terms of the eld amplitude, which correspondingly

Taira, Hill, Firth, et al, 1991; see also Moore et al., 1990), anisotropy of magnetic susceptibility (Owens, this volume), and />-wave velocity anisotropy data (Byrne et al.,

In order to check the validity of the analytic results from the 1/D expansion above for the most realistic case of D = 3, we performed Monte Carlo simulation for three-

Histograms, depicting the mass susceptibility for each rock type, are shown in Figure 4. The MS distributions of wiborgite, even-grained rapakivi granite, and Svecofennian

Distinguishable change in MS values within a studied section could be seen at Skaistgirys (increasing upwards) and Remine (decreasing upwards). These changes could

Although only the image pair with ”flat” diffusion gradient, i.e., b = 0 s/mm 2 , is required for our correction, we acquired two full data sets with reversed phase- and