pub

IGSN: IEDRM00FH
place: N42°5′59.3″, E143°2′24.7″ more
physical-form: aliquot
quantity (kg): 1.095
description: This plagioclase lherzolite was collected by Eizo in 2000. Initial work was done by M. Tanimoto.
modified at 2019-06-24

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 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 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{20090609091604316.sanjeewa,
 author={{0902-1}},
 title={Aliquot with quantity 1.095 kg at \nolinkurl{/ISEI/stone storage/Room A/1F/G/5/Horoman 2000a/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090609091604316.sanjeewa}{DREAM}},
 volume={19},
 pages={20090609091604316.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090609091604316.sanjeewa},
}

<?xml version="1.0" encoding="UTF-8"?>
<acquisitions>
  <acquisition>
    <global_id>20181024115608-836572</global_id>
    <name>0902-1</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090609091604316.sanjeewa</sample_global_id>
    <sample_name>0902-1</sample_name>
    <description/>
    <place>
      <global_id>20160517143530-817870</global_id>
      <name>locality of 0902-1</name>
      <longitude>143.040194444444</longitude>
      <latitude>42.0998055555556</latitude>
      <elevation/>
      <description/>
    </place>
    <chemistries>
      <analysis>
        <nickname>FeOT</nickname>
        <value>8.02</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181003120020-365899</global_id>
    <name>0902-1</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>20090609091604316.sanjeewa</sample_global_id>
    <sample_name>0902-1</sample_name>
    <description/>
    <place>
      <global_id>20160517143530-817870</global_id>
      <name>locality of 0902-1</name>
      <longitude>143.040194444444</longitude>
      <latitude>42.0998055555556</latitude>
      <elevation/>
      <description/>
    </place>
    <chemistries>
      <analysis>
        <nickname>B</nickname>
        <value>0.19</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Zr</nickname>
        <value>0.22</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Hf</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nb</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ta</nickname>
        <value>0.0004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181002155139-752900</global_id>
    <name>0902-1</name>
    <device>XRF PANalytical PW2400</device>
    <technique>XRF procedures of Takei (2002)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090609091604316.sanjeewa</sample_global_id>
    <sample_name>0902-1</sample_name>
    <description/>
    <place>
      <global_id>20160517143530-817870</global_id>
      <name>locality of 0902-1</name>
      <longitude>143.040194444444</longitude>
      <latitude>42.0998055555556</latitude>
      <elevation/>
      <description/>
    </place>
    <chemistries>
      <analysis>
        <nickname>SiO2</nickname>
        <value>43.6</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>TiO2</nickname>
        <value>0.02</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Al2O3</nickname>
        <value>1.56</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cr2O3</nickname>
        <value>0.38</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>FeO</nickname>
        <value>8.02</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MnO</nickname>
        <value>0.13</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>43.79</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>NiO</nickname>
        <value>0.31</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>1.57</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Na2O</nickname>
        <value>0.01</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>0.001</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>0.92</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>total</nickname>
        <value>100.4</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20181003120544-927559</global_id>
    <name>0902-1</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>20090609091604316.sanjeewa</sample_global_id>
    <sample_name>0902-1</sample_name>
    <description/>
    <place>
      <global_id>20160517143530-817870</global_id>
      <name>locality of 0902-1</name>
      <longitude>143.040194444444</longitude>
      <latitude>42.0998055555556</latitude>
      <elevation/>
      <description/>
    </place>
    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>1.44</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Rb</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sr</nickname>
        <value>0.25</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Y</nickname>
        <value>0.41</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cs</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>0.37</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>La</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ce</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pr</nickname>
        <value>0.004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Eu</nickname>
        <value>0.004</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Gd</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>0.05</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>0.02</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>0.06</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>0.09</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb</nickname>
        <value>0.023</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Th</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>U</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>

name

physical-form

quantity

0902-1 pub

powder

20090618092645318.sanjeewa

0902-1 pub

thin section

20090925091708501.sanjeewa

0902-1 pub

20180202132231-583099

place quantity

ISEI/stone storage/Room A/1F/G/--/Horoman 2000a over 1 year

2021-01-04 14:51 2022-05-20 04:46

description:

ISEI/main/127/C/3/Horoman 2000a about 5 years

2015-12-15 10:06 2021-01-04 14:51

description:

ISEI/main/127/B/1/Horoman 2000a about 1 month

2015-11-06 17:32 2015-12-15 10:06

description:

ISEI/main/127/Horoman 2000a 9 minutes

2015-11-06 17:23 2015-11-06 17:32

description:

ISEI/main/--/Horoman 2000a 1 day

2015-11-05 14:00 2015-11-06 17:23

description:

name	device	global-id
0902-1 pub 1	XRF PANalytical PW2400	20181024115608-836572
0902-1 pub 5	Q-ICPMS Agilent 7500cs	20181003120020-365899
0902-1 pub 14	XRF PANalytical PW2400	20181002155139-752900
0902-1 pub 23	Q-ICPMS Agilent 7500cs	20181003120544-927559
0902-1 pub 1 on 0902-1 pub	Q-ICPMS Agilent 7500cs	20181210102506-943342
0902-1 pub 1 on 0902-1 pub	HR-ICPMS Finningan, Element	20181210105131-365794
0902-1 pub 1 on 0902-1 pub	Thermo Scientific MAT253	20181211105611-636075
0902-1 pub 1 on 0902-1 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181211111328-502974
0902-1 pub 1 on 0902-1 pub	Q-ICPMS Agilent 7500cs	20181212104337-689616
0902-1 pub 3 on 0902-1 pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181210113352-001106
0902-1 pub 2 on 0902-1 pub	Q-ICPMS Agilent 7500cs	20181130100645-270620
0902-1 pub 2 on 0902-1 pub	MC-ICP-MS Finnigan, Neptune	20181211102803-507086
0902-1 pub 1 on 0902-1 pub	MC-ICP-MS Finnigan, Neptune	20181211111538-563402
0902-1 pub 6 on 0902-1 pub	EPMA JEOL JXA-8800R	20181128124257-566387
0902-1 pub 2 on 0902-1 pub	Thermo Scientific MAT253	20181130122357-114710

	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 1. Major element compositions of the Horoman peridotites		20091214105156539.sanjeewa

		name		spots	global-id
		0902-1.JPG pub		0	20090609091607660.sanjeewa