pub

IGSN: IEDRM00FU
physical-form: aliquot
quantity (g): 40.37
description: This plagioclase lherzolite was collected by Eizo in 2000 (a drilled core sample). Leave 20090609091553892.sanjeewa on 2015-10-15.; Leave 20111021140541-639-676 on 2015-10-16.
modified at 2019-06-18

Table 1. Major element compositions of the Horoman peridotites < 20181002155357-035338 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: 0901-1 16: 0902-1 17: 0904-2 18: 0901-2 19: 0901-3 20: 0902-3 21: 0902-10 22: 0903-13 23: HR+55 24: HR+20 25: HR+12 26: HR+0 27: HR-37 28: HR-50 29: HR-60 30: HR-70 31: HR-90 32: HR+5

(a) XRF procedures of Takei (2002) on XRF PANalytical PW2400

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 2. Trace element compositions of the Horoman samples < 20181003120730-255298 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

(a) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs

Table 3. Pb isotopic composition of the Horoman samples < 20181003143947-011557 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: 0901-1 16: 0904-2 17: 0901-2 18: 0902-3 19: 0902-10 20: 0903-13 21: HR+55 22: HR+20 23: HR+12 24: HR+0 25: HR-37 26: HR-50 27: HR-60 28: HR-70 29: HR-90 30: HR+5

(a) Pb isotopes_procedures of Makishima et al., (2007) on MC-ICP-MS Finnigan, Neptune

Table 4. Nd and Hf isotopic compositions of the Horoman samples < 20181004140110-522374 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2021-06-02

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: HR+55 16: HR+20 17: HR+12 18: HR+0 19: HR-37 20: HR-50 21: HR-60 22: HR-70 23: HR-90 24: HR+5

(a) Nd isotopes_procedures of Nakamura et al. (1991, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI

(b) Hf isotopes_procedures of Lu et al. (2007) on MC-ICP-MS Finnigan, Neptune

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 S1 . Modal abundances of minerals in the Horoman peridotites < 20181128103409-089107 > in Lalindra V. Ranaweera et al. (2018)refreshed at 2020-07-30

1: 0901-4 2: 0901-4a 3: 0901-4b 4: 0901-4c ts 5: 0902-2 6: 0902-2a 7: 0902-8 8: 0902-8a 9: 0902-8b 10: 0902-8c 11: 0904-1 12: 0904-1a 13: 0904-1b 14: 0904-1c 15: 0901-1 16: 0902-1 17: 0904-2 18: 0901-2 19: 0901-3 20: 0902-3 21: 0902-10 22: 0903-13 23: HR+55 24: HR+20 25: HR+12 26: HR+0 27: HR-37 28: HR-50 29: HR-60 30: HR-70 31: HR-90 32: HR+5

(a) EPMA on EPMA JEOL JXA-8800R

Table S2. Elemental and isotope abundances of the Horoman peridotites < 20181211095123-164197 > in Lalindra V. Ranaweera et al. (2018)refreshed at 2020-07-30

(a) Ion chromatography with pyrohydrolysis on Q-ICPMS Agilent 7500cs

(b) IRMS with TCEA on Thermo Scientific MAT253

(d) oxidation of S into sulfate (Makishima et al., 2001) on HR-ICPMS Finningan, Element

(e) Sr isotopes_procedures of Yoshikawa and Nakamura (1993) on TIMS Finnigan MAT261, MAT262 and Triton TI

(f) Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006) on Q-ICPMS Agilent 7500cs

(g) Pb=2*Pb/(Ce+Pr) on Q-ICPMS Agilent 7500cs

(h) Li isotopes_procedures of Moriguti and Nakamura (1998) on MC-ICP-MS Finnigan, Neptune

(i) IRMS with LF on Thermo Scientific MAT253

(j) Pb isotopes_procedures of Makishima et al., (2007) on MC-ICP-MS Finnigan, Neptune

(k) TIMS with double spike correction on TIMS Thermo-Fisher MAT261

(l) Nd isotopes_procedures of Nakamura et al. (1991, 2003) on TIMS Finnigan MAT261, MAT262 and Triton TI

(m) Hf isotopes_procedures of Lu et al. (2007) on MC-ICP-MS Finnigan, Neptune

@article{20090611091911347.sanjeewa,
 author={{HR-50}},
 title={Aliquot with quantity 40.37 g at \nolinkurl{/ISEI/stone storage/Room A/1F/G/7/Horoman 2010A/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090611091911347.sanjeewa}{DREAM}},
 volume={19},
 pages={20090611091911347.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090611091911347.sanjeewa},
}

<?xml version="1.0" encoding="UTF-8"?>
<acquisitions>
  <acquisition>
    <global_id>20181001151419-538409</global_id>
    <name>HR-50</name>
    <device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
    <technique>Sr isotopes_procedures of Yoshikawa and Nakamura (1993)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Rb</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sr</nickname>
        <value>7.8</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sr87zSr86</nickname>
        <value>0.702443</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Rb87zSr86</nickname>
        <value>0.011</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181024115609-947737</global_id>
    <name>HR -50</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>FeOT</nickname>
        <value>10.09</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181003120022-811765</global_id>
    <name>HR -50</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>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>B</nickname>
        <value>0.12</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Zr</nickname>
        <value>7.35</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Hf</nickname>
        <value>0.21</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nb</nickname>
        <value>0.16</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ta</nickname>
        <value>0.013</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181002155142-639000</global_id>
    <name>HR -50</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>SiO2</nickname>
        <value>43.8</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>TiO2</nickname>
        <value>0.19</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Al2O3</nickname>
        <value>3.39</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cr2O3</nickname>
        <value>0.41</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>FeO</nickname>
        <value>10.09</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MnO</nickname>
        <value>0.14</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>37.6</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>NiO</nickname>
        <value>0.25</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>3.76</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Na2O</nickname>
        <value>0.26</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>K2O</nickname>
        <value>0.004</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>P2O5</nickname>
        <value>0.007</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>-0.01</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>total</nickname>
        <value>99.8</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181003120549-255907</global_id>
    <name>HR -50</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>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>2.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Rb</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sr</nickname>
        <value>8.25</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Y</nickname>
        <value>3.78</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cs</nickname>
        <value>0.0003</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>0.23</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>La</nickname>
        <value>0.22</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ce</nickname>
        <value>0.86</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pr</nickname>
        <value>0.18</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>1.17</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.43</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Eu</nickname>
        <value>0.17</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Gd</nickname>
        <value>0.63</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.11</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>0.74</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>0.16</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>0.46</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.06</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>0.42</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.06</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb</nickname>
        <value>0.21</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Th</nickname>
        <value>0.012</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>U</nickname>
        <value>0.003</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181004135957-482357</global_id>
    <name>HR -50</name>
    <device>MC-ICP-MS Finnigan, Neptune</device>
    <technique>Hf isotopes_procedures of Lu et al. (2007)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description></description>
    <chemistries>
      <analysis>
        <nickname>Hf</nickname>
        <value>0.175</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.044</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Hf176zHf177</nickname>
        <value>0.28311</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu176zHf177</nickname>
        <value>0.034</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>eHf</nickname>
        <value>11.9</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181004103530-529998</global_id>
    <name>HR -50</name>
    <device>MC-ICP-MS Finnigan, Neptune</device>
    <technique>Pb isotopes_procedures of Makishima et al., (2007)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>UzPb</nickname>
        <value>0.002</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>ThzPb</nickname>
        <value>0.002</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb206zPb204</nickname>
        <value>18.065</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb207zPb204</nickname>
        <value>15.367</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb208zPb204</nickname>
        <value>37.674</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181004140012-659262</global_id>
    <name>HR -50</name>
    <device>TIMS Finnigan MAT261, MAT262 and Triton TI</device>
    <technique>Nd isotopes_procedures of Nakamura et al. (1991, 2003)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Nd</nickname>
        <value>1.181</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.456</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd143zNd144</nickname>
        <value>0.513028</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm147zNd144</nickname>
        <value>0.234</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>eNd</nickname>
        <value>7.6</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181011122911-778878</global_id>
    <name>HR -50</name>
    <device>EPMA JEOL JXA 8500 system</device>
    <technique>EPMA</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090611091911347.sanjeewa</sample_global_id>
    <sample_name>HR-50</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>modeOfCpx</nickname>
        <value>6.2</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>modeOfOpx</nickname>
        <value>25.3</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>modeOfOl</nickname>
        <value>64.8</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>modeOfPl</nickname>
        <value>2.8</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>modeOfSpl</nickname>
        <value>0.9</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>

name

physical-form

quantity

HR-50 pub

thin section

20120210093405-891-088

HR-50 pub

powder

20130411085135-542851

HR-50 pub

20180202135336-828029

place quantity

ISEI/stone storage/Room A/1F/G/--/Horoman 2010A 7 months

2021-01-04 14:54 2021-08-03 12:45

description:

ISEI/main/127/C/4/Horoman 2010A about 5 years

2015-12-15 10:06 2021-01-04 14:54

description:

ISEI/main/127/C/5/Horoman 2010A 1 minute

2015-12-15 10:04 2015-12-15 10:06

description:

ISEI/main/127/C/6/5/Horoman 2010A less than a minute

2015-12-15 10:04 2015-12-15 10:04

description:

ISEI/main/127/C/5/Horoman 2010A about 1 month

2015-11-06 17:22 2015-12-15 10:04

description:

ISEI/main/--/Horoman 2010A 1 day

2015-11-05 14:00 2015-11-06 17:22

description:

name	device	global-id
HR-50 pub 4	TIMS Finnigan MAT261, MAT262 and Triton TI	20181001151419-538409
HR -50 pub 1	XRF PANalytical PW2400	20181024115609-947737
HR -50 pub 5	Q-ICPMS Agilent 7500cs	20181003120022-811765
HR -50 pub 14	XRF PANalytical PW2400	20181002155142-639000
HR -50 pub 23	Q-ICPMS Agilent 7500cs	20181003120549-255907
HR -50 pub 5	MC-ICP-MS Finnigan, Neptune	20181004135957-482357
HR -50 pub 5	MC-ICP-MS Finnigan, Neptune	20181004103530-529998
HR -50 pub 5	TIMS Finnigan MAT261, MAT262 and Triton TI	20181004140012-659262
HR -50 pub 5	EPMA JEOL JXA 8500 system	20181011122911-778878
HR-50 pub 7 on HR-50 pub	EPMA JEOL JXA-8800R	20181128124259-862760
HR-50 pub 1 on HR-50 pub	Q-ICPMS Agilent 7500cs	20181210102508-460459
HR-50 pub 1 on HR-50 pub	HR-ICPMS Finningan, Element	20181210105132-464056
HR-50 pub 1 on HR-50 pub	Thermo Scientific MAT253	20181211105612-245371
HR-50 pub 1 on HR-50 pub	Q-ICPMS Agilent 7500cs	20181212104338-794548
HR-50 pub 2 on HR-50 pub	Q-ICPMS Agilent 7500cs	20181130100646-254658
HR-50 pub 2 on HR-50 pub	MC-ICP-MS Finnigan, Neptune	20181211102803-598397
HR-50 pub 2 on HR-50 pub	Thermo Scientific MAT253	20181130122358-068856

	name		global-id
	Lalindra V. Ranaweera et al. (2018) Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif, Scientific Reports, 8, doi:10.1038/s41598-018-28219-x. Table S2. Elemental and isotope abundances of the Horoman peridotites Table S1 . Modal abundances of minerals in the Horoman peridotites		20181128101201-565661
	Sanjeewa P. K. Malaviarachchi et al. (2008) Highly unradiogenic lead isotope ratios from the Horoman peridotite in Japan, Nature Geoscience, 1, 859 - 863, doi:10.1038/ngeo363. Table 2. Trace element compositions of the Horoman samples Table 4. Nd and Hf isotopic compositions of the Horoman samples Table 3. Pb isotopic composition of the Horoman samples Table 1. Major element compositions of the Horoman peridotites		20091214105156539.sanjeewa
	Malaviarachchi et al. (2010) Melt-peridotite reactions and fluid metasomatism in the upper mantle, revealed from the geochemistry of peridotite and gabbro from the Horoman peridotite massif, Japan, Journal of Petrology, 51, 1417-1445, doi:10.1093/petrology/egq024. Table 7. Sr isotopic compositions of the Horoman samples Table 1. Mineral modal compositions of the Horoman samples		20150914192726-611012

		name		spots	global-id
		HR-50.JPG pub		0	20090611091913635.sanjeewa