... Las curvas dentro de las diferentes zonas frecuentemente pueden ser interpretadas usando una aproximaci?n 1D, Moscow State University 27 Geoscan-M Ltd. ...
5. http://geophys.geol.msu.ru/shevnin/publ/180.pdf
... and Bm(kr , k ), can be found using the boundary conditions, ~ ~ ~ ~ U m(kr , k , zm) = U m+1 (kr , k , zm), (kr , k , zm). (26) (27) ~ ~ j~z,m(kr , k , zm) = j~z, m+1 Using the conditions far from the source point, i.e. ~ ~ U 0 (kr , k , z) 0, ~ ~ U N(kr ...
6. http://geophys.geol.msu.ru/berd/IPSE719.pdf
... MAGNETOVARIATIONAL SOUNDING: NEW POSSIBILITIES CR 0 1 2 345 6 719 DP , m 1230 869 614 WV 78 9 10 WC 11 12 HC 13 14 15 10 434 307 217 154 109 76.8 54.3 20 30 z, km 38.4 27.2 19.2 13.6 9.60 6.79 4.80 40 50 3.39 2.40 1.70 1.20 0.85 0.60 0.42 60 70 50 ...
7. http://geophys.geol.msu.ru/berd/IPSE722.pdf
... 299 35 45 70 147 2520 2030 12 1280 18 36 215 46 612 110 22 22 4700 754 1190 110 24 42 1220 12 22 170 27 47 280 z, km 200 100 (d) 0 0.3 5.1 41 171 46 40 3 280 30 , m 10 000 3000 1000 300 100 30 10 3 1 z, km 50 100 WV 0 CR 1 2 3 150 WC HC 200 DP km 45 ...