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Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis
of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block,
Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin,
https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Figure DR1: Diagram of classification of amphiboles (a and b) (Leake et al., 2003; Hawthorne
and Oberti, 2007)
Figure DR2: The Ab-An-Or triangular diagram of classification (Parsons, 2010)
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Table DR1 major(wt%) and trace element(ppm) analysis result of granitic rocks from Dulongjiang pluton
Sample
Granodiorite
N: 27°47.450′ E: 98°31.588′ N: 27°47.858′ E: 98°30.331′ N: 27°49.170′ E: 98°27.153′ N: 27°52.191′ E: 98°25.995′
DLJ-39 DLJ-40 DLJ-41 DLJ-44 DLJ-49 DLJ-71 DLJ-82 DLJ-87 DLJ-100 DLJ-101 DLJ-105
SiO2 64.00 63.68 63.17 65.35 65.86 63.41 63.55 61.93 62.74 63.03 59.88
TiO2 0.52 0.53 0.53 0.49 0.44 0.54 0.45 0.59 0.45 0.44 0.47
Al2O3 15.87 16.13 16.37 15.71 15.98 16.45 16.66 15.87 17.60 17.06 18.66
MgO 2.48 2.62 2.57 2.41 2.04 2.63 2.16 3.32 2.13 2.11 2.91
Fe2O3T 5.55 5.40 5.68 5.28 4.70 5.59 4.85 6.77 5.00 4.76 5.57
CaO 4.61 4.61 4.72 4.47 4.18 4.87 4.51 5.47 5.12 5.11 5.21
Na2O 2.47 2.51 2.64 2.68 2.73 2.70 2.77 2.59 2.91 2.84 2.66
K2O 2.52 2.48 2.95 2.77 3.07 2.57 3.50 2.11 2.79 2.67 2.73
MnO 0.10 0.10 0.10 0.10 0.10 0.11 0.10 0.15 0.10 0.10 0.11
P2O5 0.13 0.13 0.12 0.12 0.12 0.12 0.12 0.11 0.13 0.14 0.13
LOI 1.52 1.51 0.95 0.76 0.77 1.23 1.25 0.95 0.91 1.37 1.37
total 99.77 99.68 99.80 100.14 99.98 100.23 99.92 99.86 99.89 99.63 99.70
Li 37.2 39.7 28.9 32.9 31.0 25.6 37.1 41.8 27.5 22.7 23.7
Be 1.95 2.10 1.99 2.01 1.94 2.01 2.09 1.69 1.92 1.89 1.97
Sc 16.4 18.9 18.8 15.9 15.7 16.6 16.2 24.4 14.4 16.5 18.1
V 116 126 127 122 108 125 103 170 105 105 112
Cr 17.1 16.3 17.1 18.8 14.6 15.7 13.0 33.0 17.7 12.9 17.9
Co 27.6 27.5 33.3 31.9 35.3 33.8 25.8 29.7 33.7 30.4 29.3
Ni 3.16 3.06 3.06 4.77 2.65 6.85 5.52 8.43 7.80 6.86 6.84
Cu 18.4 14.0 14.0 11.6 7.02 8.15 22.3 153 7.82 9.23 13.9
Zn 89.8 100 88.6 81.7 86.9 98.4 68.7 85.3 86.3 216 121
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Ga 17.6 18.1 18.0 17.6 17.5 18.1 17.5 17.8 18.2 17.6 17.9
Ge 1.14 1.18 1.36 1.38 1.29 1.35 1.49 1.34 1.32 1.29 1.36
As 2.23 2.13 1.92 1.48 1.99 4.59 1.16 1.39 1.10 3.22 16.1
Rb 132 136 142 137 134 113 164 128 131 122 119
Sr 290 290 295 284 324 322 342 313 418 413 384
Y 22.4 22.8 22.9 19.3 16.7 18.8 17.6 22.9 17.1 16.6 19.5
Zr 59.5 67.7 65.5 48.2 75.9 62.1 56.7 70.3 52.2 65.6 56.1
Nb 12.8 13.0 12.6 12.7 11.1 12.8 11.8 12.2 10.2 10.6 17.9
Mo 0.99 0.83 0.56 0.42 0.46 0.84 0.20 0.76 0.66 1.13 5.08
Cs 3.52 3.26 5.35 5.16 4.05 2.12 5.94 3.10 3.24 2.22 2.85
Ba 350 326 456 409 456 401 542 345 516 574 469
La 49.3 46.5 44.2 58.7 46.7 19.9 29.8 24.0 40.9 19.1 30.2
Ce 89.1 85.4 80.5 93.5 79.3 38.3 54.7 49.0 75.0 37.6 56.4
Pr 9.20 8.67 8.29 9.76 7.91 4.30 5.63 5.68 7.32 4.13 5.55
Nd 30.2 28.8 27.9 30.0 24.2 15.5 19.3 21.1 24.6 15.4 19.5
Sm 5.18 5.06 4.73 4.69 3.87 3.33 3.51 4.26 3.79 2.94 3.69
Eu 0.93 0.96 0.95 0.85 0.84 0.80 0.84 0.95 0.86 0.77 0.84
Gd 4.29 4.54 4.31 3.78 3.33 3.01 3.30 4.24 3.29 2.82 3.46
Tb 0.62 0.65 0.64 0.55 0.48 0.49 0.47 0.61 0.49 0.44 0.53
Dy 3.63 3.61 3.70 3.04 2.73 2.93 2.65 3.57 2.77 2.61 3.07
Ho 0.70 0.71 0.73 0.61 0.52 0.61 0.56 0.73 0.57 0.55 0.63
Er 2.13 2.21 2.22 1.95 1.60 1.83 1.62 2.19 1.69 1.60 1.93
Tm 0.32 0.32 0.31 0.28 0.22 0.27 0.24 0.31 0.25 0.25 0.28
Yb 1.96 2.10 2.11 1.79 1.51 1.74 1.59 2.03 1.66 1.55 1.87
Lu 0.30 0.31 0.31 0.28 0.21 0.28 0.25 0.30 0.24 0.23 0.27
Hf 1.77 2.05 1.83 1.63 1.92 2.03 1.62 1.73 1.63 1.93 1.70
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Ta 1.41 1.26 1.42 1.48 0.90 1.26 1.19 0.99 1.21 1.24 0.34
W 107 93.5 145 151 168 78.2 115 90.5 172 82.3 2.87
Tl 0.6 0.58 0.6 0.67 0.59 0.47 0.67 0.54 0.55 0.53 0.52
Pb 18.1 18.0 18.7 18.6 17.5 15.8 16.6 12.0 18.4 19.1 16.7
Bi 0.056 0.078 0.095 0.10 0.05 0.04 0.154 0.307 0.144 0.023 0.015
Th 30.0 29.0 28.3 24.7 37.8 15.8 12.7 10.4 18.0 13.6 17.1
U 3.89 3.11 3.24 2.19 5.89 4.4 2.29 1.34 2.47 3.79 3.03
Mg# 51.0 53.0 51.3 51.5 50.3 52.3 51.0 53.4 49.8 50.8 54.9
A/CNK 1.05 1.06 1.02 1.01 1.04 1.02 1.01 0.96 1.03 1.01 1.11
Na2O/K2O 0.98 1.01 0.89 0.97 0.89 1.05 0.79 1.23 1.04 1.06 0.98
REE 197.86 189.84 180.90 209.79 173.42 93.29 124.46 118.96 163.44 89.99 128.23
LREE/HREE 19.48 18.16 17.05 23.68 22.85 10.45 15.86 11.21 20.31 11.45 13.95
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Table DR1: Continued
Sample
Enclave
N: 27°47.450′ E: 98°31.588′ N: 27°47.858′ E: 98°30.331′ N: 27°51.451′ E: 98°26.807′
DLJ-19 DLJ-20 DLJ-23 DLJ-24 DLJ-58 DLJ-59 DLJ-63 DLJ-64 DLJ-88 DLJ-89 DLJ-91
SiO2 50.00 57.44 50.83 52.27 51.73 52.02 51.70 51.65 57.70 58.36 58.54
TiO2 0.78 0.80 0.93 0.79 0.77 0.77 0.78 0.79 0.71 0.73 0.69
Al2O3 18.54 15.51 18.57 18.08 19.24 19.26 19.32 19.41 16.84 16.73 16.85
MgO 5.20 4.21 5.48 5.03 4.78 4.75 4.81 4.77 3.92 3.89 3.82
Fe2O3T 10.07 8.66 10.53 9.76 9.29 9.31 9.25 9.52 7.69 7.56 7.38
CaO 7.31 7.15 6.69 7.27 7.12 7.16 7.07 7.07 6.09 6.07 6.09
Na2O 2.62 2.86 2.89 2.89 3.29 3.33 3.37 3.25 2.88 2.84 2.93
K2O 2.82 2.23 3.00 2.00 2.27 2.17 2.08 2.08 1.65 1.73 1.79
MnO 0.24 0.23 0.24 0.23 0.23 0.23 0.23 0.22 0.17 0.17 0.17
P2O5 0.16 0.16 0.14 0.17 0.15 0.16 0.16 0.15 0.12 0.12 0.12
LOI 1.09 0.61 0.87 1.24 1.08 0.74 1.10 1.14 1.71 1.62 1.44
total 100.05 99.87 100.15 99.73 99.96 99.90 99.86 100.05 99.50 99.83 99.81
Li 33.8 32.9 59.3 32.1 51.7 43.1 47.1 44.6 46.1 47.7 45.6
Be 2.58 2.69 2.22 2.77 2.53 2.56 2.55 2.44 1.89 1.88 1.88
Sc 41.6 28.2 39.6 31.9 30.7 33.6 31.6 29.0 27.0 28.7 27.5
V 236 250 323 251 234 238 232 229 196 202 190
Cr 25.7 21.9 43.1 22.7 30.1 18.8 22.4 17.0 31.2 35.3 34.6
Co 32.6 34.3 36.1 42.2 30.3 31.6 31.7 30.2 33.4 29.7 31.2
Ni 13.8 9.64 8.95 9.61 15.6 9.79 16.9 12.3 8.52 8.62 12.1
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Cu 70.4 86.3 17.3 75.4 15.2 16.8 15.8 16.0 19.9 20.2 24.0
Zn 158 130 146 135 132 129 138 134 110 124 136
Ga 21.7 20.1 22.0 21.8 22.5 22.2 22.1 21.8 19.5 19.5 18.9
Ge 2.05 1.99 1.78 1.94 1.73 1.73 1.67 1.62 1.37 1.36 1.46
As 3.34 1.76 1.5 1.85 1.03 1.51 2.69 1.72 1.35 2.16 3.14
Rb 130 118 175 122 164 136 146 147 121 125 134
Sr 291 273 296 284 322 322 307 313 319 313 323
Y 55.2 46.2 40.9 49.1 38.3 40.0 36.3 35.1 25.2 25.4 25.9
Zr 38.8 42.4 52.1 56.0 50.6 56.1 51.5 55.5 46.8 44.1 33.4
Nb 18.8 18.7 17.4 18.1 16.1 15.3 15.3 15.2 12.7 13.5 12.4
Mo 0.55 0.67 0.72 0.83 0.56 0.49 1.18 0.73 0.82 1.75 1.52
Cs 4.80 5.32 6.6 5.65 14.3 8.18 8.98 8.44 3.61 3.65 4.16
Ba 387 239 613 201 337 355 349 332 375 383 391
La 13.7 25.0 19.7 20.8 20.6 17.8 11.1 24.0 13.6 16.3 28.7
Ce 43.8 66.5 48.0 56.4 47.3 43.1 29.8 53.1 31.2 35.2 59
Pr 6.98 8.2 6.23 7.85 6.03 5.79 4.46 6.67 4.18 4.51 6.8
Nd 32.2 33.3 26.9 33.1 25.0 24.7 20.9 26.2 17.8 18.3 25.5
Sm 8.47 7.91 6.62 7.93 6.18 6.36 5.52 6.16 4.36 4.26 5.12
Eu 1.60 1.48 1.37 1.57 1.29 1.22 1.18 1.23 0.97 0.99 1.00
Gd 8.45 7.39 6.70 7.76 5.92 6.19 5.60 5.87 4.43 4.49 4.60
Tb 1.41 1.22 1.07 1.26 0.99 1.03 0.94 0.91 0.65 0.68 0.73
Dy 8.65 7.39 6.55 7.81 5.99 6.26 5.76 5.77 3.97 4.05 4.30
Ho 1.72 1.49 1.34 1.56 1.21 1.27 1.21 1.17 0.82 0.82 0.88
Er 5.28 4.66 4.16 4.99 3.67 3.90 3.56 3.51 2.32 2.36 2.49
Tm 0.78 0.71 0.59 0.74 0.56 0.57 0.54 0.51 0.32 0.33 0.37
Yb 5.28 4.73 3.96 4.96 3.60 3.88 3.59 3.49 2.19 2.17 2.30
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Lu 0.78 0.71 0.57 0.74 0.55 0.57 0.52 0.51 0.31 0.32 0.32
Hf 1.6 1.76 1.79 2.09 1.66 1.70 1.72 1.75 1.21 1.22 1.12
Ta 1.51 1.92 1.33 1.57 1.24 1.21 2.09 1.51 0.89 3.07 1.35
W 42.5 47.1 54.1 94.5 45.5 54.5 44.8 60.3 102 68.5 75
Tl 0.54 0.59 0.78 0.56 0.75 0.63 0.70 0.66 0.51 0.54 0.62
Pb 16.7 15.9 17.1 15.7 15.9 15.1 15.7 15.3 11.4 11.2 12.7
Bi 0.17 0.20 0.18 0.16 0.20 0.27 0.11 0.10 0.14 0.10 0.09
Th 2.80 11.0 5.95 11.3 7.03 5.73 3.12 8.74 3.87 5.03 10.2
U 1.87 6.96 1.74 2.09 2.23 1.77 2.14 2.13 1.10 1.05 1.31
Mg# 54.6 53.1 54.8 54.6 54.5 54.3 54.8 53.9 54.3 54.5 54.7
A/CNK 0.90 0.77 0.92 0.90 0.92 0.92 0.94 0.95 0.96 0.95 0.95
Na2O/K2O 0.93 1.29 0.96 1.45 1.45 1.54 1.62 1.56 1.74 1.64 1.64
REE 139.10 170.69 133.75 157.47 128.89 122.65 94.68 139.10 87.13 94.78 142.11
LREE/HREE 4.82 7.16 6.33 6.14 6.78 6.02 4.87 7.76 7.23 7.83 11.48
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Table DR2 Whole-rock Rb-Sr and Sm-Nd isotopic data for granodiorite and their enclaves from Dulongjiang pluton Sample 87Sr/86Sr 2sm Sr(ppm) Rb(ppm) 143Nd/144Nd 2sm Nd(ppm) Sm(ppm) t2DM(Ga) εNd(t) Isr
DLJ-23 0.714006 0.000015 296 175 0.512093 0.000011 26.9 6.62 1.48 -9.8 0.710843
DLJ-58 0.713454 0.000008 322 164 0.512118 0.000004 25 6.18 1.45 -9.4 0.710729
DLJ-59 0.713648 0.000014 322 136 0.512085 0.000016 24.7 6.36 1.50 -10.1 0.711389
DLJ-89 0.712618 0.000015 313 125 0.512038 0.000010 18.3 4.26 1.55 -10.8 0.710482
DLJ-39 0.714903 0.000014 290 132 0.511991 0.000012 30.2 5.18 1.57 -11.2 0.712581
DLJ-49 0.713671 0.000012 324 134 0.511988 0.000013 24.2 3.87 1.57 -11.1 0.711561
DLJ-71 0.713615 0.000019 322 113 0.512025 0.000010 15.5 3.33 1.55 -10.9 0.711824
DLJ-100 0.711876 0.000014 418 131 0.512129 0.000040 24.6 3.79 1.37 -8.3 0.710277 87Rb/86Sr and 147Sm/144Nd ratios were calculated using Rb, Sr, Sm and Nd contents analyzed by ICP-MS.
T2DM represent the two-stage model age and were calculated using present-day (147Sm/144Nd)DM=0.2137, (147Sm/144Nd)DM=0.51315 and (147Sm/144Nd)crust=0.1012. εNd(t)
values were calculated using present-day (147Sm/144Nd)CHUR=0.1967 and (147Sm/144Nd)CHUR=0.512638. εNd(t)=[(143Nd/144Nd) sample(t)/(143Nd/144Nd)CHUR(t)-1]×104,
T2DM=1/λ×{1+[(143Nd/144Nd)sample-((147Sm/144Nd)sample-(147Sm/144Nd)crust) ×(eλt-1)-(143Nd/144Nd)DM]/((147Sm/144Nd)crust-(147Sm/144Nd)DM)}
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Table DR3 Single-grain zircon Hf isotopic data for the Dulongjiang pluton Grain spot Age (Ma) 176Yb/177Hf 2SE 176Lu/177Hf 2SE 176Hf/177Hf 2SE (176Hf/177Hf)i fLu/Hf εHf(0) εHf(t) 2SE TDM1(Ma) TDM2(Ma)
Enclave N:27°47.450′E:98°31.588′
DLJ19-01 128 0.069621 0.001638 0.002361 0.000046 0.282673 0.000035 0.282668 -0.93 -3.50 -0.89 1.25 851 1237
DLJ19-02 128 0.048442 0.000374 0.001419 0.000009 0.282561 0.000018 0.282558 -0.96 -7.46 -4.77 0.65 990 1484
DLJ19-03 133 0.026439 0.000266 0.000894 0.000012 0.282490 0.000019 0.282488 -0.97 -9.97 -7.14 0.69 1076 1637
DLJ19-04 134 0.025313 0.000138 0.000972 0.000006 0.282433 0.000033 0.282430 -0.97 -11.99 -9.14 1.17 1158 1765
DLJ19-05 134 0.030161 0.000175 0.001147 0.000006 0.282393 0.000027 0.282390 -0.97 -13.41 -10.57 0.97 1220 1855
DLJ19-06 134 0.021288 0.000205 0.000863 0.000007 0.282524 0.000037 0.282522 -0.97 -8.76 -5.90 1.31 1027 1560
DLJ19-07 134 0.056101 0.000309 0.002063 0.000009 0.282605 0.000054 0.282600 -0.94 -5.90 -3.15 1.91 943 1385
DLJ19-08 133 0.043375 0.000293 0.001646 0.000008 0.282515 0.000038 0.282511 -0.95 -9.09 -6.32 1.36 1062 1585
DLJ19-09 129 0.048514 0.000717 0.001774 0.000024 0.282474 0.000034 0.282469 -0.95 -10.55 -7.87 1.21 1125 1681
DLJ19-10 131 0.034690 0.000654 0.001284 0.000024 0.282719 0.000043 0.282716 -0.96 -1.88 0.88 1.51 762 1127
DLJ19-11 134 0.028016 0.000135 0.000983 0.000010 0.282461 0.000017 0.282458 -0.97 -11.01 -8.16 0.59 1119 1703
DLJ19-12 133 0.029979 0.000198 0.001140 0.000008 0.282440 0.000025 0.282438 -0.97 -11.72 -8.91 0.88 1152 1749
DLJ19-13 132 0.041201 0.000361 0.001106 0.000008 0.282503 0.000016 0.282500 -0.97 -9.53 -6.73 0.57 1064 1611
DLJ19-14 131 0.076395 0.000331 0.002363 0.000005 0.282625 0.000021 0.282619 -0.93 -5.19 -2.53 0.73 922 1344
Granodiorite N:27°47.318′E:98°31.133′
DLJ-31-01 123 0.031691 0.000274 0.001053 0.000009 0.282471 0.000013 0.282469 -0.97 -10.64 -8.03 0.44 1107 1686
DLJ-31-02 125 0.031898 0.000178 0.001116 0.000015 0.282444 0.000015 0.282441 -0.97 -11.61 -8.96 0.52 1147 1747
DLJ-31-03 125 0.035919 0.000840 0.001271 0.000039 0.282451 0.000018 0.282448 -0.96 -11.35 -8.72 0.65 1142 1731
DLJ-31-04 124 0.091348 0.000361 0.003550 0.000015 0.282662 0.000023 0.282653 -0.89 -3.90 -1.47 0.80 898 1271
DLJ-31-05 122 0.045548 0.000457 0.001507 0.000014 0.282534 0.000014 0.282530 -0.95 -8.43 -5.87 0.49 1031 1549
DLJ-31-06 122 0.070022 0.000863 0.001969 0.000015 0.282674 0.000019 0.282669 -0.94 -3.48 -0.96 0.65 842 1238
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
DLJ-31-07 120 0.043563 0.000801 0.001587 0.000027 0.282518 0.000033 0.282515 -0.95 -8.98 -6.47 1.16 1055 1585
DLJ-31-08 122 0.036272 0.000300 0.001164 0.000007 0.282452 0.000014 0.282450 -0.96 -11.31 -8.73 0.50 1137 1729
DLJ-31-09 125 0.023380 0.000255 0.000773 0.000008 0.282513 0.000011 0.282512 -0.98 -9.15 -6.47 0.40 1040 1589
DLJ-31-10 122 0.033742 0.000241 0.001108 0.000007 0.282470 0.000015 0.282468 -0.97 -10.67 -8.09 0.53 1110 1689
DLJ-31-11 124 0.038771 0.000356 0.001263 0.000011 0.282504 0.000015 0.282501 -0.96 -9.49 -6.87 0.53 1067 1614
DLJ-31-12 122 0.044922 0.000797 0.001433 0.000024 0.282576 0.000016 0.282573 -0.96 -6.92 -4.36 0.57 968 1453
DLJ-31-13 123 0.042010 0.000371 0.001308 0.000012 0.282613 0.000017 0.282610 -0.96 -5.61 -3.02 0.59 913 1369
DLJ-31-14 124 0.042951 0.000264 0.001409 0.000006 0.282505 0.000018 0.282501 -0.96 -9.45 -6.85 0.64 1069 1612
DLJ-31-15 124 0.029976 0.000116 0.000980 0.000007 0.282498 0.000012 0.282496 -0.97 -9.68 -7.04 0.43 1066 1624
DLJ-31-16 125 0.028111 0.000249 0.000848 0.000012 0.282366 0.000017 0.282364 -0.97 -14.37 -11.71 0.61 1248 1920
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
TABLE DR4: Representative major element analyses(wt.%) of amphiobole and plagioclase crystals DLJ46 host granodiorite
Sample SiO2 K2O CaO TiO2 Na2O Al2O3 SrO MgO NiO FeOT MnO Cr2O3 Total Mg# Pressure(kbar)
DLJ46-AMP Amphibole
AMP-1 49.25 0.40 11.80 0.41 0.55 6.15 0.06 12.85 0.02 14.66 0.75 0.07 96.97 60.97 2.09
AMP-2 45.99 0.58 11.89 0.79 0.98 8.57 0.12 12.01 0.00 15.55 0.66 0.04 97.17 57.92 4.17
AMP-3 46.74 0.60 11.68 0.76 0.91 8.46 0.11 12.13 0.00 15.26 0.62 0.01 97.30 58.63 4.04
AMP-4 46.11 0.58 11.69 0.77 0.87 8.75 0.12 11.42 0.02 15.91 0.59 0.02 96.86 56.14 4.35
AMP-5 47.11 0.52 11.82 0.61 0.78 7.60 0.11 11.88 0.00 15.20 0.74 0.06 96.41 58.20 3.38
AMP-6 46.73 0.52 11.88 0.71 0.72 7.87 0.16 12.20 0.04 15.25 0.65 0.05 96.77 58.77 3.59
AMP-7 53.33 0.08 12.16 0.19 0.30 2.85 0.21 14.71 0.05 12.98 0.75 0.04 97.65 66.89 -
AMP-9 45.78 0.71 11.49 0.65 0.77 8.59 0.19 11.53 0.06 16.06 0.72 0.03 96.58 56.12 4.26
AMP-10 45.84 0.73 11.70 0.71 0.84 8.90 0.11 11.21 0.00 16.76 0.66 0.01 97.46 54.39 4.47
AMP-11 46.29 0.64 11.66 0.73 0.77 8.69 0.14 11.48 0.00 16.32 0.58 0.06 97.35 55.63 4.27
AMP-15 45.66 0.63 11.49 0.84 0.93 8.82 0.06 11.33 0.04 16.25 0.63 0.11 96.78 55.41 4.43
AMP-16 47.33 0.51 11.90 0.62 0.67 7.73 0.14 11.74 0.04 15.89 0.77 0.08 97.40 56.84 3.44
AMP-20 47.08 0.49 11.72 0.62 0.70 7.61 0.11 12.05 0.12 15.14 0.74 0.00 96.38 58.65 3.39
AMP-21 47.43 0.53 11.85 0.68 0.78 7.74 0.16 12.33 0.00 15.21 0.70 0.01 97.41 59.09 3.43
AMP-22 44.58 0.69 11.67 0.88 0.86 9.63 0.16 10.87 0.02 16.85 0.60 0.06 96.87 53.48 5.16
AMP-23 47.83 0.47 11.88 0.58 0.65 7.51 0.14 12.22 0.00 15.49 0.71 0.01 97.47 58.44 3.23
AMP-24 46.76 0.54 11.67 0.71 0.78 8.00 0.07 12.02 0.01 16.01 0.64 0.01 97.21 57.25 3.68
AMP-25 45.93 0.62 11.65 0.66 0.71 8.48 0.17 11.12 0.01 16.16 0.63 0.06 96.19 55.10 4.18
DLJ46-Pl plagioclase
PL-1 60.19 0.13 7.39 0.06 6.08 26.02 0.20 0.01 0.00 0.21 0.00 0.05 100.33
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
PL-2 60.06 0.10 7.70 0.00 6.04 26.34 0.22 0.00 0.00 0.13 0.00 0.05 100.64
PL-3 56.05 0.08 11.08 0.00 4.47 29.19 0.22 0.00 0.00 0.10 0.00 0.00 101.19
PL-4 55.38 0.08 10.78 0.00 4.59 28.91 0.19 0.00 0.00 0.16 0.02 0.01 100.12
PL-5 51.14 0.03 14.68 0.00 2.60 32.38 0.19 0.00 0.00 0.12 0.00 0.00 101.13
PL-6 47.77 0.01 17.90 0.07 2.04 31.83 0.30 0.02 0.02 0.44 0.00 0.01 100.40
PL-7 51.67 0.07 13.69 0.00 3.17 31.33 0.29 0.02 0.00 0.15 0.00 0.05 100.42
PL-9 50.58 0.01 15.11 0.01 2.55 32.83 0.24 0.00 0.00 0.13 0.00 0.01 101.49
PL-10 54.06 0.05 11.81 0.02 4.19 29.83 0.32 0.00 0.00 0.09 0.00 0.11 100.48
PL-11 50.28 0.10 13.69 0.00 2.43 30.16 0.14 0.01 0.06 0.10 0.00 0.03 97.00
PL-12 54.38 0.05 11.86 0.01 3.80 30.04 0.24 0.01 0.01 0.13 0.01 0.04 100.56
PL-13 56.53 0.00 10.61 0.05 4.65 28.88 0.23 0.00 0.00 0.14 0.04 0.03 101.15
PL-14 56.45 0.12 10.49 0.00 4.65 28.30 0.26 0.00 0.00 0.15 0.00 0.06 100.48
PL-15 54.28 0.04 11.52 0.00 4.02 29.09 0.21 0.01 0.02 0.15 0.00 0.07 99.39
PL-16 55.62 0.10 11.22 0.00 4.53 28.97 0.26 0.00 0.00 0.15 0.00 0.01 100.85
PL-17 55.84 0.11 11.11 0.00 4.16 29.14 0.30 0.03 0.02 0.15 0.00 0.03 100.88
PL-18 56.12 0.11 10.71 0.00 4.31 28.70 0.16 0.01 0.00 0.15 0.03 0.04 100.32
PL-19 56.86 0.08 9.76 0.00 5.05 27.98 0.25 0.01 0.00 0.12 0.02 0.06 100.20
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Table DR4: Continued DLJ21 enclaves
Sample SiO2 K2O CaO TiO2 Na2O Al2O3 SrO MgO NiO FeOT MnO Cr2O3 Total Mg# Pressure(kbar)
DLJ21-AMP Amphibole
AMP1 44.81 0.81 11.70 0.75 0.73 8.84 0.07 10.52 0.00 17.51 0.61 0.02 96.37 51.71 4.55
AMP2 45.25 0.80 11.65 0.95 0.85 8.70 0.12 10.91 0.06 17.31 0.60 0.00 97.19 52.90 4.36
AMP3 45.53 0.67 11.64 0.87 0.79 8.29 0.09 11.02 0.02 16.51 0.64 0.02 96.09 54.32 4.05
AMP4 45.05 0.78 11.59 0.87 0.80 8.82 0.07 10.71 0.00 17.05 0.54 0.02 96.28 52.82 4.51
AMP5 45.60 0.84 11.37 0.88 0.78 8.44 0.12 10.81 0.02 17.53 0.54 0.02 96.96 52.36 4.14
AMP6 46.01 0.63 11.63 0.75 0.64 8.51 0.09 10.82 0.05 17.07 0.56 0.06 96.81 53.04 4.18
AMP10 46.70 0.60 11.75 0.71 0.73 7.43 0.16 11.62 0.02 16.60 0.60 0.03 96.95 55.51 3.25
AMP11 46.75 0.55 11.66 0.56 0.68 7.28 0.10 11.54 0.00 16.10 0.59 0.06 95.86 56.11 3.17
AMP12 46.37 0.58 11.82 0.55 0.69 7.46 0.13 11.38 0.02 16.45 0.59 0.04 96.10 55.23 3.34
AMP13 47.26 0.61 11.79 0.46 0.62 7.31 0.12 11.30 0.05 16.20 0.55 0.04 96.30 55.42 3.17
AMP14 45.93 0.67 11.77 0.60 0.71 7.94 0.18 11.10 0.04 17.38 0.60 0.03 96.94 53.24 3.73
AMP15 46.04 0.65 11.94 0.64 0.73 8.34 0.11 10.79 0.03 17.18 0.60 0.08 97.13 52.81 4.04
DLJ21-AMP plagioclase inclusion
AMP7 57.19 0.03 9.60 0.00 4.91 28.01 0.18 0.02 0.02 0.38 0.02 0.02 100.38
AMP8 56.91 0.07 10.09 0.00 4.97 28.04 0.19 0.00 0.02 0.33 0.00 0.05 100.66
AMP9 54.89 0.03 11.58 0.00 4.36 29.35 0.26 0.00 0.00 0.33 0.00 0.06 100.85
DLJ61-AMP Amphibole
AMP-1 47.50 0.54 11.75 0.68 0.70 7.51 0.14 12.10 0.00 15.44 0.63 0.01 97.00 58.26 3.27
AMP-1 47.19 0.54 11.96 0.60 0.71 7.40 0.16 12.04 0.03 15.39 0.59 0.04 96.65 58.25 3.21
AMP-2 47.19 0.50 11.73 0.59 0.71 7.55 0.14 11.99 0.00 15.31 0.61 0.20 96.52 58.27 3.33
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
AMP-3 46.82 0.37 11.50 0.83 0.86 7.97 0.18 11.50 0.04 15.99 0.71 0.07 96.84 56.18 3.69
AMP-4 46.41 0.52 11.70 0.84 0.84 8.00 0.13 11.71 0.00 15.39 0.67 0.05 96.26 57.56 3.74
AMP-5 47.71 0.44 11.44 0.86 0.81 7.71 0.10 12.67 0.00 14.26 0.61 0.03 96.63 61.29 3.40
AMP-6 47.54 0.42 11.93 0.81 0.76 7.81 0.12 12.81 0.00 14.23 0.67 0.00 97.08 61.61 3.47
AMP-9 48.00 0.38 11.67 0.79 0.80 7.56 0.15 13.49 0.03 13.75 0.61 0.04 97.27 63.62 3.23
AMP-10 47.73 0.40 11.61 0.86 0.83 7.71 0.16 12.92 0.06 13.53 0.56 0.01 96.37 63.00 3.41
AMP-11 46.88 0.44 11.74 0.89 0.77 8.07 0.21 12.51 0.00 14.59 0.60 0.01 96.71 60.45 3.74
AMP-12 47.78 0.45 11.90 0.76 0.76 7.27 0.15 12.46 0.01 15.34 0.67 0.04 97.58 59.14 3.03
AMP-13 48.37 0.49 11.95 0.60 0.71 6.85 0.14 12.69 0.02 14.63 0.65 0.09 97.19 60.71 2.67
AMP-14 46.82 0.55 11.76 0.64 0.65 7.74 0.13 11.97 0.00 15.62 0.67 0.01 96.54 57.74 3.50
AMP-15 47.28 0.52 11.92 0.59 0.64 7.59 0.19 12.10 0.00 15.16 0.64 0.00 96.62 58.72 3.35
AMP-19 46.45 0.60 11.65 0.63 0.84 7.65 0.09 11.77 0.00 15.37 0.75 0.03 95.81 57.72 3.48
AMP-20 47.09 0.55 11.63 0.61 0.75 7.77 0.14 11.97 0.00 15.45 0.54 0.00 96.48 58.00 3.52
AMP-21 46.67 0.55 11.66 0.60 0.80 8.00 0.16 11.81 0.00 15.86 0.70 0.00 96.80 57.04 3.71
AMP-22 47.12 0.56 11.96 0.72 0.65 7.35 0.09 12.66 0.00 14.99 0.59 0.00 96.69 60.09 3.15
DLJ21-AMP plagioclase inclusion
AMP-16 57.65 0.07 9.18 0.00 5.26 27.65 0.25 0.00 0.00 0.34 0.03 0.03 100.44 AMP-17 49.50 0.00 15.49 0.00 2.22 33.04 0.23 0.00 0.00 0.42 0.00 0.02 100.91 AMP-18 56.81 0.07 9.32 0.00 5.28 27.26 0.20 0.00 0.00 0.40 0.03 0.00 99.36 DLJ61-Pl plagioclase
PL-1 56.95 0.14 9.52 0.00 5.13 28.15 0.24 0.00 0.02 0.14 0.00 0.02 100.31
PL-2 56.05 0.07 10.64 0.02 4.77 28.61 0.18 0.00 0.01 0.15 0.00 0.00 100.50
PL-3 58.14 0.14 8.71 0.00 5.41 27.22 0.24 0.00 0.00 0.19 0.01 0.00 100.05
PL-4 57.33 0.09 9.10 0.00 5.19 27.45 0.26 0.02 0.02 0.11 0.00 0.06 99.62
PL-5 51.86 0.04 13.50 0.00 3.16 31.48 0.26 0.01 0.00 0.09 0.00 0.04 100.45
PL-6 56.44 0.12 9.77 0.02 4.77 28.06 0.29 0.00 0.00 0.17 0.02 0.09 99.74
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
PL-7 57.19 0.08 9.41 0.00 5.16 27.62 0.24 0.00 0.04 0.11 0.02 0.04 99.90
PL-8 52.91 0.08 12.72 0.00 3.57 30.41 0.18 0.03 0.00 0.11 0.03 0.02 100.05
PL-9 55.77 0.05 10.80 0.00 4.57 28.91 0.29 0.00 0.02 0.08 0.00 0.00 100.49
PL-10 54.29 0.04 11.92 0.00 3.90 29.73 0.21 0.00 0.01 0.14 0.00 0.00 100.24
PL-11 55.53 0.11 10.39 0.00 4.42 28.47 0.27 0.00 0.01 0.17 0.01 0.01 99.40
PL-12 55.94 0.14 10.12 0.00 4.96 28.62 0.24 0.01 0.00 0.20 0.00 0.04 100.26
PL-13 56.91 0.13 9.99 0.00 4.79 28.19 0.26 0.00 0.00 0.13 0.00 0.08 100.47
PL-14 50.37 0.05 14.80 0.00 2.52 32.39 0.26 0.00 0.00 0.10 0.00 0.03 100.52
PL-15 49.88 0.06 14.99 0.00 2.50 32.40 0.15 0.00 0.00 0.15 0.00 0.02 100.14
PL-16 50.72 0.07 14.83 0.00 2.51 32.24 0.18 0.02 0.11 0.20 0.01 0.00 100.86
PL-17 55.95 0.13 10.77 0.00 4.89 28.52 0.24 0.02 0.01 0.16 0.01 0.00 100.69
PL-18 56.43 0.05 10.25 0.00 4.68 28.36 0.29 0.00 0.00 0.18 0.00 0.00 100.23
PL-19 57.19 0.09 10.19 0.00 5.08 27.87 0.17 0.02 0.04 0.22 0.00 0.00 100.87
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Supplementary Dataset Results of zircon LA-ICP-MS U-Pb data
Analysis content(ppm) ratios ages(Ma)
Th U Th/U 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 208Pb/232Th 1σ 207Pb/206Pb 1σ 207Pb/235U 1σ 206Pb/238U 1σ 208Pb/232Th 1σ
Location1 DLJ31 Granodiorite (N:27°47.318′E:98°31.133′)
spot-1 741 916 0.81 0.04605 0.00213 0.12259 0.0055 0.01931 0.00022 0.00618 0.0001 99 117 5 123 1 125 2
spot-2 491 417 1.18 0.05221 0.00218 0.14093 0.0051 0.01958 0.00023 0.00624 0.0001 295 62 134 5 125 1 126 2
spot-3 1738 1354 1.28 0.05178 0.00139 0.13981 0.0026 0.01958 0.00018 0.00648 0.00006 276 26 133 2 125 1 131 1
spot-4 2074 1392 1.49 0.05118 0.00153 0.13728 0.0031 0.01945 0.00019 0.00649 0.00007 249 34 131 3 124 1 131 1
spot-5 632 646 0.98 0.04959 0.00228 0.13092 0.0054 0.01915 0.00024 0.00607 0.00011 176 72 125 5 122 2 122 2
spot-6 423 427 0.99 0.05229 0.00304 0.13827 0.0079 0.01918 0.00022 0.00602 0.00005 298 136 132 7 122 1 121.3 1
spot-7 695 459 1.51 0.04615 0.00305 0.11938 0.0078 0.01876 0.00022 0.00598 0.00008 5 146 115 7 120 1 121 2
spot-8 346 288 1.20 0.05198 0.00353 0.13743 0.0092 0.01917 0.00024 0.00602 0.00005 285 157 131 8 122 2 121.4 1
spot-9 1820 1353 1.34 0.04955 0.00221 0.13407 0.0053 0.01962 0.00024 0.00618 0.00011 174 70 128 5 125 2 125 2
spot-10 665 597 1.11 0.05057 0.00277 0.13348 0.0072 0.01914 0.00022 0.00603 0.00005 221 127 127 6 122 1 121.6 0.9
spot-11 1390 1120 1.24 0.04892 0.00287 0.13053 0.0075 0.01935 0.00022 0.00612 0.00005 144 133 125 7 124 1 123.4 1
spot-12 584 557 1.05 0.04839 0.00237 0.12754 0.0056 0.01911 0.00024 0.00573 0.0001 118 78 122 5 122 2 115 2
spot-13 439 416 1.05 0.05218 0.00301 0.13843 0.0078 0.01924 0.00023 0.00604 0.00005 293 134 132 7 123 1 121.7 1
spot-14 654 587 1.11 0.05243 0.00179 0.14062 0.0039 0.01945 0.0002 0.00604 0.00008 304 45 134 3 124 1 122 2
spot-15 1513 1073 1.41 0.05029 0.00285 0.13422 0.0075 0.01936 0.00022 0.00611 0.00005 208 131 128 7 124 1 123 0.9
spot-16 525 749 0.70 0.05347 0.00171 0.14388 0.0037 0.01952 0.0002 0.00666 0.00009 349 39 136 3 125 1 134 2
spot-17 317 379 0.84 0.04605 0.00199 0.11926 0.0049 0.01878 0.00023 0.00618 0.00018 92 114 4 120 1 125 4
spot-18 228 375 0.61 0.05197 0.00225 0.14016 0.0054 0.01956 0.00023 0.00636 0.00013 284 66 133 5 125 1 128 3
spot-19 1271 1001 1.27 0.05099 0.00247 0.13291 0.0058 0.0189 0.00024 0.00585 0.0001 240 77 127 5 121 2 118 2
spot-20 996 1005 0.99 0.05046 0.00217 0.1348 0.0051 0.01937 0.00023 0.00628 0.00011 216 66 128 5 124 1 127 2
spot-21 748 435 1.72 0.05117 0.0029 0.13771 0.0072 0.01952 0.00028 0.00624 0.00011 248 94 131 6 125 2 126 2
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
Location2 DLJ75 Granodiorite (N:27°47.750′E:98°27.177′)
spot-1 606 721 0.84 0.05117 0.00175 0.13599 0.0045 0.01927 0.00018 0.00607 0.00004 249 81 129 4 123 1 122.3 0.9
spot-2 564 573 0.98 0.05276 0.00193 0.1403 0.005 0.01929 0.00018 0.00605 0.00004 318 85 133 4 123 1 121.9 0.9
spot-3 262 290 0.90 0.0525 0.00279 0.13875 0.0072 0.01917 0.00022 0.00601 0.00005 307 124 132 6 122 1 121.2 1
spot-4 867 623 1.39 0.04865 0.00132 0.13098 0.0025 0.01952 0.00018 0.00583 0.00005 131 28 125 2 125 1 117 1
spot-5 792 879 0.90 0.04825 0.0013 0.13002 0.0025 0.01954 0.00018 0.00559 0.00006 112 28 124 2 125 1 113 1
spot-6 297 272 1.09 0.05104 0.00243 0.13494 0.0063 0.01917 0.00021 0.00604 0.00005 243 112 129 6 122 1 121.6 0.9
spot-7 351 375 0.94 0.05214 0.00201 0.13964 0.0052 0.01943 0.00019 0.0061 0.00005 291 90 133 5 124 1 122.9 0.9
spot-8 440 420 1.05 0.0519 0.00141 0.13957 0.0027 0.0195 0.00018 0.00608 0.00006 281 28 133 2 124 1 123 1
spot-9 582 1405 0.41 0.05212 0.00115 0.14089 0.0017 0.0196 0.00017 0.00615 0.00006 291 13 134 2 125 1 124 1
spot-10 497 635 0.78 0.05228 0.00135 0.14063 0.0025 0.0195 0.00018 0.00682 0.00007 298 24 134 2 124 1 137 1
spot-11 327 408 0.80 0.05047 0.00145 0.13472 0.0029 0.01935 0.00019 0.00602 0.00007 217 32 128 3 124 1 121 1
spot-12 856 707 1.21 0.04988 0.00123 0.13367 0.0022 0.01943 0.00018 0.00574 0.00005 189 21 127 2 124 1 116 1
spot-13 482 666 0.72 0.04918 0.00121 0.13202 0.0021 0.01946 0.00018 0.00599 0.00006 156 21 126 2 124 1 121 1
spot-14 580 1237 0.47 0.04989 0.00136 0.13182 0.0026 0.01916 0.00018 0.0061 0.00008 190 29 126 2 122 1 123 2
spot-15 376 490 0.77 0.04786 0.00125 0.12811 0.0024 0.01941 0.00018 0.00598 0.00006 92 26 122 2 124 1 121 1
spot-16 825 1027 0.80 0.04914 0.00114 0.1324 0.0019 0.01953 0.00018 0.00621 0.00006 155 17 126 2 125 1 125 1
spot-17 265 314 0.84 0.04739 0.00141 0.12798 0.003 0.01958 0.0002 0.00613 0.00008 69 36 122 3 125 1 124 2
spot-18 256 404 0.63 0.04898 0.00139 0.13255 0.0028 0.01962 0.00019 0.00606 0.00007 147 32 126 3 125 1 122 1
spot-19 369 466 0.79 0.05117 0.00136 0.13821 0.0026 0.01959 0.00019 0.00608 0.00007 248 26 131 2 125 1 123 1
spot-20 255 381 0.67 0.05113 0.00157 0.13794 0.0033 0.01956 0.0002 0.00623 0.00008 247 37 131 3 125 1 126 2
spot-21 537 422 1.27 0.05241 0.00145 0.14148 0.0029 0.01957 0.00019 0.00612 0.00007 303 29 134 3 125 1 123 1
spot-22 362 410 0.88 0.05218 0.0025 0.14058 0.0065 0.01954 0.00022 0.00614 0.00005 293 112 134 6 125 1 124 1
spot-23 526 538 0.98 0.04957 0.00124 0.13394 0.0023 0.0196 0.00019 0.00605 0.00006 175 22 128 2 125 1 122 1
Location3 DLJ19 enclave (N:27°47.450′E:98°31.588′)
spot-1 301 247 0.82 0.05087 0.00668 0.14027 0.0182 0.02 0.00041 0.0063 0.00012 235 280 133 16 128 3 127 2
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
spot-2 263 194 0.74 0.05069 0.0092 0.14001 0.0251 0.02003 0.00057 0.00631 0.00018 227 344 133 22 128 4 127 4
spot-3 126 376 2.97 0.04933 0.00345 0.14204 0.0097 0.02089 0.00032 0.0066 0.00013 163 159 135 9 133 2 133 3
spot-4 214 368 1.72 0.05256 0.00264 0.15264 0.007 0.021 0.00029 0.00621 0.00013 310 80 144 6 134 2 125 3
spot-5 893 633 0.71 0.05289 0.00238 0.15338 0.0062 0.02099 0.00027 0.00584 0.00009 324 68 145 5 134 2 118 2
spot-6 588 359 0.61 0.05397 0.00284 0.15602 0.0075 0.02093 0.0003 0.00619 0.00012 370 83 147 7 134 2 125 2
spot-7 237 222 0.93 0.04629 0.00263 0.13472 0.0071 0.02108 0.0003 0.00619 0.00012 13 86 128 6 134 2 125 2
spot-8 287 368 1.28 0.05264 0.00323 0.15097 0.0091 0.0208 0.00027 0.00652 0.00006 313 143 143 8 133 2 131 1
spot-9 621 628 1.01 0.04721 0.00273 0.13154 0.0074 0.02021 0.00025 0.00643 0.00007 60 127 125 7 129 2 129 1
spot-10 577 1517 2.63 0.04929 0.00196 0.13963 0.0048 0.02052 0.00024 0.0084 0.00043 162 59 133 4 131 2 169 9
spot-11 416 1485 3.57 0.04907 0.00149 0.1424 0.0034 0.02102 0.00021 0.00623 0.00011 151 37 135 3 134 1 126 2
spot-12 366 379 1.03 0.0471 0.00301 0.13503 0.0081 0.02078 0.00032 0.00696 0.00016 54 102 129 7 133 2 140 3
spot-13 842 983 1.17 0.05217 0.00245 0.14905 0.0068 0.02072 0.00023 0.00651 0.00005 293 110 141 6 132 1 131 1
spot-14 673 430 0.64 0.05286 0.00543 0.14947 0.0148 0.0205 0.00049 0.00653 0.00024 323 180 141 13 131 3 132 5
Location4 DLJ56 enclave (N:27°47.858′E:98°30.331′)
spot-1 227 679 0.33 0.04953 0.00136 0.13775 0.0036 0.02017 0.00019 0.00637 0.00006 173 66 131 3 129 1 128 1
spot-2 504 534 0.94 0.05162 0.00245 0.14004 0.0065 0.01968 0.0002 0.00619 0.00005 268 111 133 6 126 1 124.7 1
spot-3 2418 3113 0.78 0.05014 0.00144 0.14143 0.0039 0.02046 0.00019 0.00646 0.00005 201 68 134 3 131 1 130.1 1
spot-4 881 2215 0.40 0.05146 0.00112 0.14757 0.0017 0.0208 0.00019 0.00774 0.00007 261 12 140 1 133 1 156 1
spot-5 206 236 0.87 0.05234 0.0033 0.14566 0.009 0.02018 0.00024 0.00634 0.00006 300 146 138 8 129 2 128 1
spot-6 1104 967 1.14 0.05188 0.00244 0.1426 0.0065 0.01994 0.00021 0.00626 0.00005 280 110 135 6 127 1 126.2 0.9
spot-7 239 305 0.78 0.05343 0.00155 0.15309 0.0033 0.02078 0.00021 0.00717 0.00008 347 31 145 3 133 1 144 2
spot-8 287 502 0.57 0.05098 0.00217 0.13875 0.0057 0.01974 0.00021 0.00622 0.00006 240 101 132 5 126 1 125 1
spot-9 204 256 0.80 0.05359 0.00251 0.15391 0.0065 0.02083 0.00027 0.00648 0.00013 354 71 145 6 133 2 131 3
spot-10 346 444 0.78 0.04974 0.00215 0.1378 0.0058 0.02009 0.00021 0.00635 0.00005 183 101 131 5 128 1 128 1
spot-11 329 416 0.79 0.05094 0.00202 0.14306 0.0055 0.02037 0.00021 0.00641 0.00005 238 94 136 5 130 1 129 1
spot-12 932 1101 0.85 0.05264 0.0019 0.15005 0.0045 0.02067 0.00023 0.00628 0.00009 313 48 142 4 132 1 127 2
Zhu, R.-Z., Lai, S.-C., Qin, J.-F., Zhao, S.-W., and Santosh, M., 2019, Petrogenesis of high-K calc-alkaline granodiorite and its enclaves from the SE Lhasa block, Tibet (SW China): Implications for recycled subducted sediments: GSA Bulletin, https://doi.org/10.1130/B31841.1.
GSA Data Repository Item 2019034
spot-13 148 212 0.70 0.05232 0.0023 0.1468 0.0063 0.02035 0.00022 0.00639 0.00005 300 103 139 6 130 1 129 1