Skip to main content

Table 6 Summary of zircon (U–Th)/He data

From: Thermochronology of hydrothermal alteration zones in the Kii Peninsula, southwest Japan: an attempt for detecting the thermal anomalies and implications to the regional exhumation history

Sample code

Grain ID

Mass [μm]

238U [ppm]

232Th [ppm]

Th/U

4He [ncc/mg]

FT

eU [ppm]

(U-Th)/He age ± 1σ [Ma]

Raw

Corr

Unknown

Weighted mean age ± 1σ:

16.8 ± 3.9

HJG1-0 m

008

2.8

–

–

–

1665.3

–

–

–

–*

015

1.3

302.0

162.7

0.54

477.4

0.60

340.3

11.5

19.3 ± 2.2

HJG1-1 m

010

2.8

481.2

242.7

0.50

827.8

0.71

538.2

12.6

17.8 ± 2.0

003

2.4

584.4

294.2

0.50

489.0

0.71

653.5

6.2

8.7 ± 1.0

HJG1-3 m

008

2.2

256.8

129.0

0.50

374.1

0.69

287.1

10.7

15.5 ± 1.7

004

3.7

570.2

212.8

0.37

910.8

0.75

620.2

12.1

16.2 ± 1.8

HJG1-10 m

009

3.1

901.1

292.4

0.32

1539.6

0.74

969.8

13.0

17.7 ± 2.0

013

4.0

605.4

147.6

0.24

585.9

0.73

640.1

7.5

10.3 ± 1.2

HJG1-20 m

006

4.9

312.7

181.5

0.58

652.0

0.75

355.4

15.1

20.2 ± 2.3

010

6.2

163.7

68.9

0.42

901.2

0.77

179.8

41.1

53.4 ± 6.0**

HJG2-0 m

002

4.6

147.2

128.0

0.87

210.9

0.76

177.3

9.8

12.8 ± 1.4

004

5.7

171.6

110.2

0.64

438.1

0.77

197.5

18.2

23.6 ± 2.6

HJG2-1 m

006

1.9

573.4

372.7

0.65

956.0

0.68

660.9

11.9

17.4 ± 1.9

009

1.7

483.1

481.1

1.00

864.2

0.64

596.2

11.9

18.5 ± 2.1

HJG2-3 m

003

5.3

659.8

179.8

0.27

1295.3

0.76

702.0

15.2

20.0 ± 2.2

010

2.2

274.5

133.2

0.49

415.8

0.70

305.8

11.2

15.9 ± 1.8

HJG2-10 m

006

3.7

5122.1

12,243.4

2.39

635.9

0.73

7999.3

0.7

0.9 ± 0.1**

009

3.8

309.1

176.4

0.57

554.9

0.72

350.5

13.0

18.1 ± 2.0

Fish Canyon Tuff: 28.3 ± 0.4 Ma (ZHe age ± 1σ; Gleadow et al. 2015)

Weighted mean age ± 1σ:

27.7 ± 3.1

FCT3

013

5.1

217.9

93.5

0.43

978.0

0.76

239.9

19.7

24.5

103

9.8

356.9

213.0

0.60

1106.5

0.80

406.9

22.3

27.8

108

4.5

342.0

182.1

0.53

1066.0

0.74

384.8

22.7

30.7

  1. aFT is the α-ejection correlation (Farley et al. 1996; Hourigan et al. 2005). Proxy for alpha-radiation activity is computed as eU = [U] + 0.235[Th] (Shuster et al. 2006). [*sample lost during U–Th measurement; **not included in weighted mean calculations; Corr., corrected; eU, effective uranium concentration]