pub

IGSN: IEDRM00G1
place: N42°6′25.6″, 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 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 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 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{20090714090744146.sanjeewa,
 author={{0901-4a}},
 title={Fraction at \nolinkurl{/ISEI/stone storage/Room A/1F/A/0/Horoman 2000v/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20090714090744146.sanjeewa}{DREAM}},
 volume={19},
 pages={20090714090744146.sanjeewa},
 year={2009},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20090714090744146.sanjeewa},
}

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    <global_id>20181003120019-928856</global_id>
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        <nickname>Zr</nickname>
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        <nickname>Nb</nickname>
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        <unit>ppm</unit>
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        <nickname>Ta</nickname>
        <value>0.004</value>
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  <acquisition>
    <global_id>20181002155135-724402</global_id>
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        <nickname>SiO2</nickname>
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      <analysis>
        <nickname>TiO2</nickname>
        <value>0.12</value>
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      <analysis>
        <nickname>Al2O3</nickname>
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        <unit>%</unit>
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      <analysis>
        <nickname>Cr2O3</nickname>
        <value>0.37</value>
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      <analysis>
        <nickname>FeO</nickname>
        <value>8.09</value>
        <unit>%</unit>
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      <analysis>
        <nickname>MnO</nickname>
        <value>0.13</value>
        <unit>%</unit>
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        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>38.28</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>NiO</nickname>
        <value>0.26</value>
        <unit>%</unit>
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      <analysis>
        <nickname>CaO</nickname>
        <value>3.23</value>
        <unit>%</unit>
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        <label/>
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      <analysis>
        <nickname>Na2O</nickname>
        <value>0.32</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>K2O</nickname>
        <value>0.009</value>
        <unit>%</unit>
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        <label/>
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      <analysis>
        <nickname>P2O5</nickname>
        <value>0.006</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>0.8</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>total</nickname>
        <value>100.4</value>
        <unit>%</unit>
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  <acquisition>
    <global_id>20181003120538-877478</global_id>
    <name>0901-4a</name>
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    <sample_global_id>20090714090744146.sanjeewa</sample_global_id>
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      <global_id>20160517143439-838212</global_id>
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      <longitude>143.046611111111</longitude>
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      <analysis>
        <nickname>Li</nickname>
        <value>1.79</value>
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      <analysis>
        <nickname>Rb</nickname>
        <value>0.03</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Sr</nickname>
        <value>8.03</value>
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        <nickname>Y</nickname>
        <value>3.01</value>
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        <nickname>Cs</nickname>
        <value>0.001</value>
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        <nickname>Ba</nickname>
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        <unit>ppm</unit>
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        <nickname>Sm</nickname>
        <value>0.22</value>
        <unit>ppm</unit>
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        <nickname>Eu</nickname>
        <value>0.09</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Gd</nickname>
        <value>0.36</value>
        <unit>ppm</unit>
        <uncertainty/>
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      <analysis>
        <nickname>Tb</nickname>
        <value>0.07</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Dy</nickname>
        <value>0.54</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Ho</nickname>
        <value>0.12</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
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        <nickname>Er</nickname>
        <value>0.35</value>
        <unit>ppm</unit>
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        <label/>
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      <analysis>
        <nickname>Tm</nickname>
        <value>0.05</value>
        <unit>ppm</unit>
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      <analysis>
        <nickname>Yb</nickname>
        <value>0.37</value>
        <unit>ppm</unit>
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        <nickname>Lu</nickname>
        <value>0.06</value>
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        <nickname>Pb</nickname>
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        <unit>ppm</unit>
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        <nickname>Th</nickname>
        <value>0.004</value>
        <unit>ppm</unit>
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        <nickname>U</nickname>
        <value>0.002</value>
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        <nickname>ThzPb</nickname>
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        <nickname>Sm</nickname>
        <value>0.228</value>
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        <nickname>Nd143zNd144</nickname>
        <value>0.513676</value>
        <unit></unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>Sm147zNd144</nickname>
        <value>0.298</value>
        <unit></unit>
        <uncertainty/>
        <label/>
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      <analysis>
        <nickname>eNd</nickname>
        <value>20.0</value>
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name

physical-form

quantity

0901-4a pub

powder

20090619091305580.sanjeewa

0901-4a pub

thin section

20120124092018-632-749

0901-4a pub

powder

20180202131918-268745

place quantity

ISEI/stone storage/Room A/1F/A/0/Horoman 2000v almost 3 years

2018-09-20 09:41 2021-08-03 11:34

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
0901-4a pub 1 on 0901-4a pub	Q-ICPMS Agilent 7500cs	20181210102506-869687
0901-4a pub 1 on 0901-4a pub	HR-ICPMS Finningan, Element	20181210105131-570089
0901-4a pub 1 on 0901-4a pub	Q-ICPMS Agilent 7500cs	20181212104336-935343
0901-4a pub 3 on 0901-4a pub	TIMS Finnigan MAT261, MAT262 and Triton TI	20181210113351-980984
0901-4a pub 2 on 0901-4a pub	MC-ICP-MS Finnigan, Neptune	20181211102802-024118
0901-4a pub 2 on 0901-4a pub	Q-ICPMS Agilent 7500cs	20181130100644-232414
0901-4a pub 1 on 0901-4a pub	MC-ICP-MS Finnigan, Neptune	20181211112917-239149
0901-4a pub 1 on 0901-4a pub	Thermo Scientific MAT253	20181211105611-810960
0901-4a pub 1	XRF PANalytical PW2400	20181024115608-531133
0901-4a pub 5	Q-ICPMS Agilent 7500cs	20181003120019-928856
0901-4a pub 14	XRF PANalytical PW2400	20181002155135-724402
0901-4a pub 23	Q-ICPMS Agilent 7500cs	20181003120538-877478
0901-4a pub 5	MC-ICP-MS Finnigan, Neptune	20181004103528-892701
0901-4a pub 5	TIMS Finnigan MAT261, MAT262 and Triton TI	20181004140010-606842
0901-4a pub 7 on 0901-4a pub	EPMA JEOL JXA-8800R	20181128124253-850056
0901-4a pub 2 on 0901-4a pub	Thermo Scientific MAT253	20181130122356-723923

	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

name	spots	global-id
0901-4a.JPG pub	0	20090714090738956.sanjeewa
0901-4a.JPG pub	0	20090715094128457.sanjeewa