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Table 1 Positions of coring sites and summary of inclination data

From: Paleomagnetic inclination variations during the last 200 kyr in the Okhotsk Sea and their relation to persistent non-axial-dipole field

Site Latitude (N) Longitude (E) Depth (m) GAD I Mean I I
GC1 + PC7 51°16.5′ 149°12.5′ 1253 68.2 71.2 3.0
GC3 52°36.1′ 150°08.3′ 1048 69.1 69.9 0.8
GC5 52°39.6′ 149°08.8′ 1084 69.1 75.0 5.9
GC6 53°13.5′ 148°56.5′ 1456 69.5 64.6 −4.9
GC8 + PC6 53°16.9′ 150°04.7′ 1145 69.5 69.2 −0.3
GC9 + PC5 54°19.0′ 149°16.1′ 828 70.2 70.9 0.7
GC10 54°43.0′ 149°17.9′ 513 70.5 70.8 0.3
GC11 53°25.7′ 148°58.3′ 1381 69.6 68.8 −0.8
GC12 53°10.4′ 148°56.5′ 1299 69.5 74.2 4.7
  1. I inclination, GAD geocentric axial dipole, ∆I inclination anomaly (observed inclination minus GAD inclination)