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176

Yb

a

176

Lu

a

178

Hf

180

Hf Sig

Hf

b 176

Hf

176

Hf

d

“ ı

c

T

DM

e

age

f

“ ı U-Pb

g

Lu-Hf

h

177

Hf

177

Hf

177

Hf

177

Hf

(V)

177

Hf

177

Hf

(t)

İ+I (Ga) (Ma) (Ma) conc seq

İ+I

(t)

d

Grain

“ ı

“ ı

±2ı

c

A108_seq4_26 0.0143 12 0.00060 4 1.46709 1.88633 7 0.281632 33 0.281609 4.2 1.2 2.18 2024 20 93 4

A112_seq4_26 0.0096 26 0.00034 9 1.46713 1.88647 8 0.280938 29 0.280922 -11.8 1.0 3.35 2388 12 92 4

A116_seq4_26 0.0710 118 0

.00244 37 1.46716 1

.88656 6 0.281643 34 0.281545 4.0 1.2 2.26 2115 15 94 4

A118_seq4_40 0.0299 24 0

.00112 7 1.46719

1.88665 9 0.281608 28 0.281567 1.1 1.0 2.29 1953 44 91 4

A123_seq4_40 0.0200 17 0.00066 4 1.46725 1.88658 12 0.280744 53 0.280706 -4.8 1.9 3.48 3012 14 90 4

A125_seq4_40 0.0198 42 0.

00058 12 1.46715 1.

88663 7 0.281602 41 0.281580 2.6 1.5 2.24 2000 22 90 4

A138_seq4_26 0.0107 9 0.00036 2 1.46707 1.88647 5 0.281279 36 0.281265 -8.2 1.3 2.85 2017 20 99 4

A145_seq4_26 0.0008 1 0.00002 0 1.46722 1.88656 5 0.281008 41 0.281007 -15.0 1.4 3.31 2118 17 93 4

A155_seq4_26 0.0162 20 0.00051 5 1.46719 1.88670 6 0.281257 29 0.281238 -10.4 1.0 2.93 1962 21 99 4

A161_seq4_26 0.0349 83 0

.00119 27 1.46711

1.88621 7 0.282213 40 0.282203 -10.1 1.4 1.69 473 5 134

4

A162_seq4_26 0

.0020 3 0.00005 1 1

.46714 1.88625 8 0.281081 31 0.281078 -8.1 1.1 3.08 2308 14 93 4

A163_seq4_26 0.0208 20 0.

00072 6 1.46705 1.

88635 6 0.281307 35 0.281279 -8.1 1.2 2.83 1999 14 102 4

A164_seq4_26 0.0210 17 0.

00076 5 1.46709 1.

88639 7 0.282178 30 0.282169 -7.1 1.1 1.68 658 4 99 4

A168_seq4_26 0.0252 21 0.00084 5 1.46713 1.88619 6 0.281044 38 0.281005 -6.4 1.4 3.14 2494 15 101 4

A175_seq4_26 0

.0074 6 0.00024 1

1.46710 1.88645 7 0.281048 25 0.281037 -6.1 0.9 3.10 2457 14 95 4

A177_seq4_26 0.0166 13 0.00058 4 1.46719 1.88628 7 0.281127 31 0.281099 -1.0 1.1 2.92 2579 13 90 4

Quoted uncertainties (absolute) relate to the last quoted figure. The effect of the inter-element fractionation on Lu/Hf was estimated to be about 6 % or less

based on analyses of the GJ-ϭ ĂŶĚ WůĞƐŽǀŝēĞ njŝƌĐŽŶ͘ ĐĐƵƌĂĐLJ ĂŶĚ ƌĞƉƌŽĚƵĐŝďŝůŝƚLJ ǁĂƐ ĐŚĞĐŬĞĚ ďLJ ƌĞƉĞĂƚĞĚ ĂŶĂůLJƐĞƐ ŽĨ ƌĞĨĞƌĞŶĐĞ njircon GJ-ϭ ĂŶĚ WůĞƐŽǀŝēĞ

(data given as mean with 2 standard deviation uncertainties).

(a)

176

Yb/

177

Hf = (

176

Yb/

173

Yb)

true

x (

173

Yb/

177

Hf)

meas

x (M

173(Yb)

/M

177(Hf)

)

ɴ;,ĨͿ

͕ ɴ;,ĨͿ с ůŶ;;

179

Hf/

177

Hf

true

)/(

179

Hf/

177

Hf

measured

)) / ln(M

179(Hf)

/M

177(Hf)

), M = mass of

respective isotopes. The

176

Lu/

177

Hf was calculated in a similar way using

175

Lu/

177

,Ĩ ĂŶĚ ɴ;zďͿ͘

(b)

Mean Hf signal in volts.

(c)

Uncertainties are quadratic additions of the within-run precision and the daily reproducibility of the 40ppb-JMC475 solution. Uncertainties for the JMC475

quoted at 2SD (2 standard deviation).

(d)

Initial

176

Hf/

177

,Ĩ ĂŶĚ ɸ,Ĩ ĐĂůĐƵůĂƚĞĚ ƵƐŝŶŐ ƚŚĞ ĂƉƉĂƌĞŶƚ h-Pb age determined by LA-ICP-MSdating (see column f), and the CHUR parameters:

176

Lu/

177

Hf =

0.0336, and

176

Hf/

177

Hf = 0.282785 (Bouvier et al. 2008).

(e)

Two stage model age in Ga using measured

176

Lu/

177

Lu of each spot (first stage = age of zircon), a value of 0.0113 for the average continental crust (second

stage, values compiled from Rudnick and Gao (2003), and depleted mantle

176

Lu/

177

Lu = 0.0379, and

176

Hf/

177

Hf = 0.283164.

(f)

Apparent U-Pb age determined by LA-ICP-MS.

(g)

U-Pb age concordance (%).

(h)

Sequence in which Lu-Hf analyses were performed. Standard analyses for each sequence are showed on Table 12.

279