- IGSN: IEDRM00GH
- physical-form: aliquot
- quantity (g): 34.82
- description: This gabbro was collected by Eizo in 2000 (a drilled core sample). Leave 20090611091755342.sanjeewa on 2015-10-15.; Leave 20111021140541-639-676 on 2015-10-16.
- modified at 2019-06-18
Table 1. Mineral modal compositions of the Horoman samples < 20181011122657-794350 > in Malaviarachchi et al. (2010)refreshed at 2021-06-02
1: 0901-4 2: 0902-2 3: 0902-8 4: 0902-8a 5: 0902-8b 6: 0902-8c 7: 0904-1 8: 0901-2 9: 0902-3 10: HR+55 11: HR+20 12: HR+12 13: HR+0 14: HR-37 15: HR-50 16: HR-60 17: HR-70 18: HR-90 19: HR+5 20: HR-10 21: HR-20 22: HR-30 23: HR-40 24: HR-80
(a) EPMA on EPMA JEOL JXA 8500 system
Table 4: Major element compositions of the Horoman samples < 20181001150755-047931 > in Malaviarachchi et al. (2010)refreshed at 2021-06-02
1: 0902-7 2: 0902-9 3: 0903-8 4: 0903-11 5: 0903-1 6: 0903-2 7: 0903-5 8: HR-10 9: HR-20 10: HR-30 11: HR-40 12: HR-80 13: 0903-6 14: 0903-7 15: 0903-9 16: 0903-10 17: 0903-12
(a) XRF procedures of Takei (2002) on XRF PANalytical PW2400
Table 5. Trace element compositions of the Horoman samples < 20181002134243-245585 > in Malaviarachchi et al. (2010)refreshed at 2021-06-03
1: 0902-7 2: 0902-9 3: 0903-8 4: 0903-11 5: 0903-1 6: 0903-2 7: 0903-5 8: HR-10 9: HR-20 10: HR-30 11: HR-40 12: HR-80 13: 0903-6 14: 0903-7 15: 0903-9 16: 0903-10 17: 0903-12
(a) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs
Table 6. Pb, Nd and Hf isotopic compositions of the Horoman samples < 20181001150835-968988 > in Malaviarachchi et al. (2010)refreshed at 2021-06-04
1: 0902-7 2: 0902-9 3: 0903-8 4: 0903-11 5: 0903-1 6: 0903-2 7: 0903-5 8: HR-10 9: HR-20 10: HR-30 11: HR-40 12: HR-80 13: 0903-6 14: 0903-7 15: 0903-9 16: 0903-10 17: 0903-12
(a) Pb isotopes_procedures of Kuritani and Nakamura (2002, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI
(b) Nd isotopes_procedures of Nakamura et al. (1991, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI
(c) Hf isotopes_procedures of Lu et al. (2007) on MC-ICP-MS Finnigan, Neptune
(d) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs
Table 7. Sr isotopic compositions of the Horoman samples < 20181001151020-495322 > in Malaviarachchi et al. (2010)refreshed at 2021-06-03
1: HR+55 2: HR+20 3: HR+12 4: HR+0 5: HR-37 6: HR-50 7: HR-60 8: HR-70 9: HR-90 10: HR+5 11: HR-10 12: HR-20 13: HR-30 14: HR-40 15: HR-80
(a) Sr isotopes_procedures of Yoshikawa and Nakamura (1993) on TIMS Finnigan MAT261, MAT262 and Triton TI
Table S3. Oxygen and lithium isotope abundances of the Horoman gabbros and Hidaka metasediments < 20181211114703-572997 > in Lalindra V. Ranaweera et al. (2018)refreshed at 2020-07-30
1: HR-10 2: HR-20 3: HR-30 4: HR-40 5: HR-80 6: 0903-6 7: 0903-7 8: 0903-9 9: 0903-10 10: 0903-12
(a) IRMS with LF on Thermo Scientific MAT253
(b) Li isotopes_procedures of Moriguti and Nakamura (1998) on MC-ICP-MS Finnigan, Neptune
@article{20090612091345540.sanjeewa,
author={{HR-30}},
title={Aliquot with quantity 34.82 g at \nolinkurl{/ISEI/stone storage/Room A/1F/G/7/Horoman 2010A/}},
journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090612091345540.sanjeewa}{DREAM}},
volume={19},
pages={20090612091345540.sanjeewa},
year={2009},
url={http://dream.misasa.okayama-u.ac.jp/?q=20090612091345540.sanjeewa},
}<?xml version="1.0" encoding="UTF-8"?>
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<nickname>Rb</nickname>
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<value>28.9</value>
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<global_id>20181002132225-880690</global_id>
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<sample_global_id>20090612091345540.sanjeewa</sample_global_id>
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<analysis>
<nickname>Hf</nickname>
<value>0.41</value>
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<value>0.11</value>
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<global_id>20181002134608-904604</global_id>
<name>HR-30</name>
<device>XRF PANalytical PW2400</device>
<technique>XRF procedures of Takei (2002)</technique>
<operator>Sanjeewa</operator>
<sample_global_id>20090612091345540.sanjeewa</sample_global_id>
<sample_name>HR-30</sample_name>
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<analysis>
<nickname>SiO2</nickname>
<value>46.4</value>
<unit>%</unit>
<uncertainty/>
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<analysis>
<nickname>TiO2</nickname>
<value>0.295</value>
<unit>%</unit>
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<analysis>
<nickname>Al2O3</nickname>
<value>7.3</value>
<unit>%</unit>
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<info/>
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<analysis>
<nickname>Cr2O3</nickname>
<value>0.325</value>
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<analysis>
<nickname>FeO</nickname>
<value>8.65</value>
<unit>%</unit>
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<analysis>
<nickname>MnO</nickname>
<value>0.143</value>
<unit>%</unit>
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<analysis>
<nickname>MgO</nickname>
<value>29.8</value>
<unit>%</unit>
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<analysis>
<nickname>NiO</nickname>
<value>0.175</value>
<unit>%</unit>
<uncertainty/>
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<analysis>
<nickname>CaO</nickname>
<value>5.96</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Na2O</nickname>
<value>0.741</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>K2O</nickname>
<value>0.01</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>P2O5</nickname>
<value>0.012</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>total</nickname>
<value>99.9</value>
<unit>%</unit>
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<acquisition>
<global_id>20181002140109-637182</global_id>
<name>HR-30</name>
<device>Q-ICPMS Agilent 7500cs</device>
<technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
<operator>Sanjeewa</operator>
<sample_global_id>20090612091345540.sanjeewa</sample_global_id>
<sample_name>HR-30</sample_name>
<description/>
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<analysis>
<nickname>Li</nickname>
<value>1.63</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>Rb</nickname>
<value>0.06</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>Sr</nickname>
<value>31.1</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
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<analysis>
<nickname>Y</nickname>
<value>6.52</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Cs</nickname>
<value>0.0003</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Ba</nickname>
<value>0.71</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>La</nickname>
<value>0.36</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Ce</nickname>
<value>1.33</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pr</nickname>
<value>0.25</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
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<analysis>
<nickname>Nd</nickname>
<value>1.59</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Sm</nickname>
<value>0.61</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Eu</nickname>
<value>0.26</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Gd</nickname>
<value>0.932</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Tb</nickname>
<value>0.179</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Dy</nickname>
<value>1.23</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Ho</nickname>
<value>0.27</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Er</nickname>
<value>0.81</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Tm</nickname>
<value>0.12</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Yb</nickname>
<value>0.75</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Lu</nickname>
<value>0.12</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb</nickname>
<value>0.23</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Th</nickname>
<value>0.01</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>U</nickname>
<value>0.003</value>
<unit>ppm</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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<acquisition>
<global_id>20181002140148-993130</global_id>
<name>HR-30</name>
<device>Q-ICPMS Agilent 7500cs</device>
<technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
<operator>Sanjeewa</operator>
<sample_global_id>20090612091345540.sanjeewa</sample_global_id>
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<nickname>B</nickname>
<value>0.08</value>
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<label/>
<info/>
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<analysis>
<nickname>Zr</nickname>
<value>10.4</value>
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<label/>
<info/>
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<analysis>
<nickname>Hf</nickname>
<value>0.35</value>
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<label/>
<info/>
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<analysis>
<nickname>Nb</nickname>
<value>0.16</value>
<unit>ppm</unit>
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<label/>
<info/>
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<analysis>
<nickname>Ta</nickname>
<value>0.01</value>
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<label/>
<info/>
</analysis>
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<acquisition>
<global_id>20181002141756-521361</global_id>
<name>HR-30</name>
<device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
<technique>Pb isotopes_procedures of Kuritani and Nakamura (2002, 2003)</technique>
<operator>Sanjeewa</operator>
<sample_global_id>20090612091345540.sanjeewa</sample_global_id>
<sample_name>HR-30</sample_name>
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<analysis>
<nickname>Pb206zPb204</nickname>
<value>18.08</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb207zPb204</nickname>
<value>15.44</value>
<unit></unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>Pb208zPb204</nickname>
<value>37.704</value>
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<label/>
<info/>
</analysis>
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<acquisition>
<global_id>20181011122912-638496</global_id>
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<technique>EPMA</technique>
<operator>Sanjeewa</operator>
<sample_global_id>20090612091345540.sanjeewa</sample_global_id>
<sample_name>HR-30</sample_name>
<description/>
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<nickname>modeOfCpx</nickname>
<value>17.2</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>modeOfOpx</nickname>
<value>22.7</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>modeOfOl</nickname>
<value>27.6</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>modeOfPl</nickname>
<value>30.3</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
<analysis>
<nickname>modeOfSpl</nickname>
<value>2.2</value>
<unit>%</unit>
<uncertainty/>
<label/>
<info/>
</analysis>
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place quantity
ISEI/stone storage/Room A/1F/G/--/Horoman 2010A 7 months
2021-01-04 14:54 2021-08-17 01:17
description:
ISEI/main/--/Horoman 2010A 1 day
2015-11-05 14:00 2015-11-06 17:22
description: