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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)