Earth, Planets and Space

Table 2 The RMS misfit against the iteration

From: Electrical conductivity of old oceanic mantle in the northwestern Pacific I: 1-D profiles suggesting differences in thermal structure not predictable from a plate cooling model

Iteration	Area A					Area B
Iteration	Total	xx	xy	yx	yy	Total	xx	xy	yx	yy
0	4.66	5.40	4.86	3.02	4.98	9.32	17.51	2.35	3.03	5.16
1	3.99	4.80	3.19	2.54	4.92	9.10	17.28	2.15	1.88	4.94
2	4.08	5.05	2.79	3.01	4.92	9.12	17.31	2.15	1.89	4.97

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