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Table 1 Paleomagnetically investigated sites in the Styrian Basin

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

Location

Latitude (°N)

Longitude (°E)

Name

N

D (°)

I (°)

k

α95 (°)

Plat (°N)

PLong (°E)

dp (°)

dm (°)

δ

(°)

Polarity

Reference

Altenmarkt bei Riegersburg, lava flow, Basanit, Pliocene, Fritz (1992)

 Altenmarkt

47.005

15.912

AM03

6

187.6

− 64.3

1276.0

1.9

− 84.7

293.7

2.4

3.0

3.3

R

This study

Stradner Kogel (Wilhelmsdorf), vent with dikes, Nephelinite, 1.71 ± 0.72, K/Ar, Balogh et al. (1994)

 Stradner Kogel

46.841

15.926

SK02

18

198.5

− 57.6

231.3

2.3

− 73.9

311.6

2.4

3.3

11.4

R

This study

 Waltra

46.849

15.952

WA02

12

204.8

− 60.6

170.1

3.3

− 71.5

293.4

3.9

5.1

12.0

R

This study

Stradner Kogel

46.847

15.935

SK

52

200.0

− 60.0

87.9

2.1

− 62.5

301.2

  

10.4

R

1

 Waltra

46.85

15.953

WA

10

213.0

− 58.0

34.0

7.6

− 64.6

292.3

  

17.0

R

2

Stein, intrusion, Basalt with Olivin, Pliocene, Balogh et al. (1994)

 Stein

46.991

16.082

ST02

11

174.7

− 61.1

289.3

2.7

− 83.9

56.2

3.2

4.1

4.6

R

This study

 Stein

46.992

16.083

ST

20

176

− 64

192

2.3

− 87

82.7

  

2.0

R

2

Klöch-Königsberg volcanic complex

Klöch Quarry, vent with dikes, Nephelinebasanite, 2.56 ± 1.2 Ma, K/Ar, Balogh et al. (1994)

 Klöch 01

46.769

15.964

KN01

7

220.0

− 30.5

96.0

6.2

− 45.2

314.9

3.8

6.9

42.3

T

This study

 Klöch 02

46.769

15.964

KN02

9

217.7

– 34.5

43.9

7.9

− 48.5

315.1

5.2

9.0

37.8

T

This study

 Klöch 03

46.77

15.964

KN03

6

217.6

− 32.9

101.3

6.7

− 47.8

316.3

4.3

7.6

39.2

T

This study

 Klöch 04

46.77

15.965

KN04

5

202.5

− 32.7

30.9

14.0

− 55.6

335.8

9.0

15.8

35.0

T

This study

 Klöch 05

46.768

15.964

KN05

7

198.6

− 39.1

18.9

14.2

− 61.2

338.2

10.2

17.0

27.9

T

This study

 Klöch 06

46.767

15.965

KN06

5

207.9

− 35.7

127.3

6.8

− 54.7

326.2

4.6

7.9

33.5

T

This study

 Klöch 07

46.767

15.965

KN07

5

217.2

− 41.9

78.3

8.7

− 52.7

310.3

6.5

10.7

31.1

T

This study

 Klöch 08

46.768

15.964

KN08

5

214.3

− 33.5

255.1

4.8

− 50.0

319.6

3.1

5.5

37.6

T

This study

 Klöch 09

46.768

15.964

KN09

3

192.6

− 47.2

180.5

9.2

− 69.1

343.3

7.7

11.9

18.9

(T)

This study

 Klöch 11

46.773

15.968

KN11

6

215.3

− 24.6

55.6

9.1

− 45.0

323.2

5.2

9.7

46.2

T

This study

 Klöch 12

46.767

15.968

KN12

9

211.6

− 40.1

69.5

6.2

− 55.2

318.3

4.5

7.5

30.7

T

This study

 Klöch 13

46.768

15.967

KN13

10

207.4

− 45.6

65.8

6.0

− 60.8

318.8

4.9

7.6

24.4

(T)

This study

 Seindl

46.763

15.953

SL

12

209.5

− 49.6

17.0

9.8

− 62.0

310.9

  

21.7

(T)

2

 Klöch SW

46.763

15.963

S1

9

211.9

− 39.9

179.0

3.5

− 54.8

317.8

  

31.0

T

2

 Klöch N

46.767

15.967

S2

39

224.4

− 28.6

25.0

4.5

− 41.5

311.1

  

45.6

T

2

 Klöch 01-13

46.769

15.965

KN01-13

83

211.5

− 37.2

39.8

2.5

− 53.6

320.6

1.7

2.9

 

T

This study

Klöch Quarry, synvolcanic lake sediment with several layers of accretionary lapilli, reddish, sandy clay, Pliocene

 Klöch 10

46.775

15.963

KN10

6

212.5

− 42.3

159.3

5.3

− 55.8

315.4

4.0

6.6

29.0

T

This study

Zaraberg, baked tuff with lava flow, Nephelinebasanite, Pliocene, Balogh et al. (1994)

 Klöch 14

46.764

15.946

KN14

8

211.8

-28.8

95.3

5.7

− 48.9

325.2

3.5

6.3

41.2

T

This study

 Klöch 15

46.764

15.946

KN15

5

219.2

− 33.5

403.2

3.8

− 47.1

314.1

2.5

4.3

39.2

T

This study

 Klöch 1415

46.764

15.946

KN14-15

13

214.6

− 30.6

106.9

4.0

− 48.4

320.9

2.5

4.5

 

T

this study

 Reichel

46.773

15.952

RL

17

222.0

− 37.3

123.0

3.1

− 47.3

308.3

  

36.9

T

2

Königsberg, tuff with dikes, 2.17 ± 0.13 Ma, K/Ar, Seghedi et al. (2004)

 Tieschen 01

46.783

15.954

TD01

13

214.4

− 33.7

85.3

4.5

− 50.1

319.4

2.9

5.1

37.4

T

This study

 Tieschen 02

46.785

15.956

TD02

9

221.2

− 39.4

275.4

3.1

− 48.9

308.1

2.2

3.7

34.7

T

This study

 Tieschen 03

46.787

15.956

TS03/TD04

17

207.9

− 42.2

71.1

4.3

− 58.4

321.4

3.2

5.2

27.6

T

This study

Neuhaus, intrusion, Basalt with Olivin, 3.76 ± 0.41 Ma and 3.11 ± 0.75 Ma, K/Ar, Balogh et al. (1994)

 Neuhaus

46.865

16.027

NH02

7

217.8

−33.4

69.2

7.3

−47.8

315.8

4.7

8.3

38.9

T

This study

 Neuhaus

46.867

16.028

NH

9

224.5

− 31.8

183.0

3.4

− 43.0

309.2

  

42.7

T

2

Steinberg (MĂ¼hldorf), vent with dikes, Olivin nephelinite, 2.64 ± 0.55 Ma, 3.05 ± 1.4 Ma, 2.30 ± 0.14 Ma, K/Ar, Balogh et al. (1994)

 Steinberg 01

46.935

15.917

SB01

9

196.8

22.1

15.5

13.5

− 29.7

356.9

7.6

14.3

88.0

T

This study

 Steinberg 02

46.935

15.917

SB02

9

201.9

35.9

79.9

5.8

− 20.3

353.9

3.9

6.7

102.3

T

This study

 Steinberg 03

46.934

15.916

SB03

10

203.6

21.7

11.3

15.0

− 28.1

349.5

8.4

15.9

88.5

T

This study

 Steinberg 04

46.935

15.918

SB04

8

196.2

36.6

52.2

7.7

− 21.1

359.6

5.3

9.0

102.3

T

This study

 Steinberg 05

46.935

15.919

SB05

10

203.7

28.2

31.3

8.8

− 24.5

350.7

5.3

9.6

95.0

T

This study

 Steinberg SB

46.935

15.917

SB01-05

46

200.7

28.8

20.8

4.7

− 25.0

353.8

2.9

5.2

95.1

T

This study

  1. For each volcanic unit the name is given together with the kind of exposure, rock type, age, its standard deviation, dating method and the reference is given. For the sites, the name of location; latitude; longitude; site name; number of samples; declination and inclination of the characteristic remanent magnetization; precision parameter and 95% confidence circle radius of the Fisher (1953) statistics; latitude and longitude of the virtual magnetic pole position with half angles of the error ellipses; reversal angle (Prévot et al. 1985); polarity (N: normal, R: reversed, T: transitional); and reference (1: Mauritsch 1972; 2: Pohl and Soffel 1982) are listed