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Table 4 Paleointensity results of the Styrian lavas

From: Intermediate field directions recorded in Pliocene basalts in Styria (Austria): evidence for cryptochron C2r.2r-1

Location

Latitude (°N)

Longitude (°E)

Name

D (°)

I (°)

α95 (°)

Plat (°N)

PLong (°E)

PI (µT)

sPI (µT)

VDM (1022 Am2)

sVDM (1022 Am2)

Altenmarkt

47.005

15.912

AM03

187.6

− 64.3

1.9

− 84.7

293.7

57.4

3.4

9.3

1.1

Stradner Kogel

46.841

15.926

SK02

198.5

− 57.6

2.3

− 73.9

311.6

22.0

 

3.9

 

Waltra

46.849

15.952

WA02

204.8

− 60.6

3.3

− 71.5

293.4

17.4

0.5

3.0

0.2

Klöch 12

46.767

15.968

KN12

211.6

− 40.1

6.2

− 55.2

318.3

12.0

2.0

2.6

0.8

Klöch 14

46.764

15.946

KN14

211.8

− 28.8

5.7

− 48.9

325.2

8.6

0.7

2.0

0.3

Klöch 15

46.764

15.946

KN15

219.2

− 33.5

3.8

− 47.1

314.1

12.9

4.2

2.9

1.9

Tieschen 01

46.783

15.954

TD01

214.4

− 33.7

4.5

− 50.1

319.4

11.2

2.5

2.6

1.1

Tieschen 03

46.787

15.956

TS03/TD04

207.9

− 42.2

4.3

− 58.4

321.4

10.5

3.9

2.2

1.6

Steinberg SB

46.935

15.917

SB01-05

200.7

28.8

4.7

− 25.0

353.8

4.9

2.6

1.1

1.2

  1. D: declination of the ChRM; I: inclination of the ChRM; α95: 95% confidence circle radius of the Fisher (1953) statistics; Plat: latitude of the VGP position; Plon: longitude of the VGP position; PI: mean paleointensity; sPI: standard deviation of paleointensity; VDM: virtual dipole moment from PI; sVDM: standard deviation of VDM