pub

IGSN: IEDRM00G8
place: N42°5′15.4″, E143°2′47.8″ more
classification: plutonic:ultramafic
physical-form: fraction
status: unknown
modified at 2019-06-25

Table 1. Major element compositions of the Horoman peridotites < 20181002155357-035338 > in Sanjeewa P. K. Malaviarachchi et al. (2008)refreshed at 2022-06-25

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 2022-06-25

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 2022-06-23

(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 2022-06-25

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 2022-06-25

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 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{20090714090900510.sanjeewa,
 author={{0904-1b}},
 title={Fraction at \nolinkurl{/ISEI/stone storage/Room A/1F/A/0/Horoman 2000v/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090714090900510.sanjeewa}{DREAM}},
 volume={19},
 pages={20090714090900510.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090714090900510.sanjeewa},
}

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        <nickname>FeOT</nickname>
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    <global_id>20181003120020-671824</global_id>
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      <analysis>
        <nickname>B</nickname>
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      <analysis>
        <nickname>Zr</nickname>
        <value>2.09</value>
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        <nickname>Hf</nickname>
        <value>0.06</value>
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        <nickname>Nb</nickname>
        <value>0.03</value>
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        <nickname>Ta</nickname>
        <value>0.002</value>
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    <global_id>20181002155138-312576</global_id>
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        <nickname>SiO2</nickname>
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        <nickname>TiO2</nickname>
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      <analysis>
        <nickname>Al2O3</nickname>
        <value>2.49</value>
        <unit>%</unit>
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      <analysis>
        <nickname>Cr2O3</nickname>
        <value>0.41</value>
        <unit>%</unit>
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      </analysis>
      <analysis>
        <nickname>FeO</nickname>
        <value>7.93</value>
        <unit>%</unit>
        <uncertainty/>
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      </analysis>
      <analysis>
        <nickname>MnO</nickname>
        <value>0.13</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>41.4</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>NiO</nickname>
        <value>0.29</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>2.03</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Na2O</nickname>
        <value>0.13</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>K2O</nickname>
        <value>0.006</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>P2O5</nickname>
        <value>0.005</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>0.6</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>total</nickname>
        <value>100.4</value>
        <unit>%</unit>
        <uncertainty/>
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  <acquisition>
    <global_id>20181003120543-575227</global_id>
    <name>0904-1b</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>20090714090900510.sanjeewa</sample_global_id>
    <sample_name>0904-1b</sample_name>
    <description/>
    <place>
      <global_id>20160517143616-807469</global_id>
      <name>locality of 0904-1</name>
      <longitude>143.046611111111</longitude>
      <latitude>42.0876111111111</latitude>
      <elevation/>
      <description/>
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    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>2.0</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Rb</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Sr</nickname>
        <value>6.15</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Y</nickname>
        <value>1.8</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cs</nickname>
        <value>0.01</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>0.23</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
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      <analysis>
        <nickname>La</nickname>
        <value>0.09</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Ce</nickname>
        <value>0.3</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
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      <analysis>
        <nickname>Pr</nickname>
        <value>0.06</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>0.39</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.14</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Eu</nickname>
        <value>0.05</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Gd</nickname>
        <value>0.21</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.04</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>0.29</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>0.07</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>0.19</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>0.23</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
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      <analysis>
        <nickname>Pb</nickname>
        <value>0.037</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Th</nickname>
        <value>0.002</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>U</nickname>
        <value>0.001</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
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    <global_id>20181004103529-879195</global_id>
    <name>0904-1b</name>
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    <technique>Pb isotopes_procedures of Makishima et al., (2007)</technique>
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      <analysis>
        <nickname>UzPb</nickname>
        <value>0.102</value>
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      <analysis>
        <nickname>ThzPb</nickname>
        <value>0.036</value>
        <unit></unit>
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      <analysis>
        <nickname>Pb206zPb204</nickname>
        <value>17.095</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
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      <analysis>
        <nickname>Pb207zPb204</nickname>
        <value>15.309</value>
        <unit></unit>
        <uncertainty/>
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        <info/>
      </analysis>
      <analysis>
        <nickname>Pb208zPb204</nickname>
        <value>36.761</value>
        <unit></unit>
        <uncertainty/>
        <label/>
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  <acquisition>
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    <technique>Hf isotopes_procedures of Lu et al. (2007)</technique>
    <operator>Sanjeewa</operator>
    <sample_global_id>20090714090900510.sanjeewa</sample_global_id>
    <sample_name>0904-1b</sample_name>
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      <global_id>20160517143616-807469</global_id>
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      <analysis>
        <nickname>Hf</nickname>
        <value>0.067</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Lu</nickname>
        <value>0.034</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Hf176zHf177</nickname>
        <value>0.28385</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu176zHf177</nickname>
        <value>0.073</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>eHf</nickname>
        <value>38.1</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
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    </chemistries>
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  <acquisition>
    <global_id>20181004140011-718256</global_id>
    <name>0904-1b</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>20090714090900510.sanjeewa</sample_global_id>
    <sample_name>0904-1b</sample_name>
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      <longitude>143.046611111111</longitude>
      <latitude>42.0876111111111</latitude>
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    <chemistries>
      <analysis>
        <nickname>Nd</nickname>
        <value>0.395</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>0.146</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd143zNd144</nickname>
        <value>0.513089</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm147zNd144</nickname>
        <value>0.224</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>eNd</nickname>
        <value>8.5</value>
        <unit></unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>

name

physical-form

quantity

0904-1b pub

powder

20090619091447914.sanjeewa

0904-1b pub

20180202133458-896287

place quantity

ISEI/stone storage/Room A/1F/A/0/Horoman 2000v almost 4 years

2018-09-20 09:41 2022-07-30 08:27

description:

ISEI/stone storage/Room A/1F/A/Horoman 2000v almost 3 years

2015-09-25 13:23 2018-09-20 09:41

description:

name	device	global-id
0904-1b pub 1 on 0904-1b pub	Thermo Scientific MAT253	20181211105611-398659
0904-1b pub 1 on 0904-1b pub	Q-ICPMS Agilent 7500cs	20181210102506-336706
0904-1b pub 1 on 0904-1b pub	HR-ICPMS Finningan, Element	20181210105131-301693
0904-1b pub 1 on 0904-1b pub	Q-ICPMS Agilent 7500cs	20181212104337-740679
0904-1b pub 3 on 0904-1b pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181210113352-457077
0904-1b pub 2 on 0904-1b pub	Q-ICPMS Agilent 7500cs	20181130100645-021748
0904-1b pub 2 on 0904-1b pub	MC-ICP-MS Finnigan, Neptune	20181211102802-457121
0904-1b pub 1	XRF PANalytical PW2400	20181024115608-445253
0904-1b pub 5	Q-ICPMS Agilent 7500cs	20181003120020-671824
0904-1b pub 14	XRF PANalytical PW2400	20181002155138-312576
0904-1b pub 23	Q-ICPMS Agilent 7500cs	20181003120543-575227
0904-1b pub 5	MC-ICP-MS Finnigan, Neptune	20181004103529-879195
0904-1b pub 5	MC-ICP-MS Finnigan, Neptune	20181004135957-038308
0904-1b pub 5	TIMS Finnigan MAT261, MAT262 and Triton TI	20181004140011-718256
0904-1b pub 2 on 0904-1b pub	Thermo Scientific MAT253	20181130122357-885666

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	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 Table 3. Pb isotopic composition of the Horoman samples Table 4. Nd and Hf isotopic compositions of the Horoman samples		20091214105156539.sanjeewa

		name		spots	global-id
		0904-1b.JPG pub		0	20090714090854222.sanjeewa