pub

info data bibtex casteml

classification: volcanic:basaltic
physical-form: hand specimen
quantity (g): 89.23
description: Stromboli island; San Bartolo effusive event between 360BC and 7AD. Sample set ST94.8 consists of melt inclusions hosted in olivine crystals recovered from lava sample ST103 (Schiavi et al., 2012)
modified at 2020-04-10

ST103

Table 1S. Major element compositions of San Bartolo lava Schiavi, Federica et al. (2011)

1: ST103

(a) EPMA on EPMA

Table 1S(a). Major element compositions of olivine grains from San Bartolo lava Schiavi, Federica et al. (2011)

1: ol2b 2: ol3g 3: ol4d 4: ol8e 5: ol59 6: ol60-1 7: ol60-2 8: ol62 9: ol64 10: ol74

(a) SEM-EDX on SEM-EDX 3100H with HORIBA EMAX

Table 1 Trace element composition of San Bartolo lava and olivine-hosted melt inclusions Schiavi, Federica et al. (2011)

1: ST103 2: MI2b 3: MI3g 4: MI4d 5: MI8e 6: MI60-1 7: MI60-2 8: MI8a 9: MI28a 10: MI50a 11: MI52a 12: MI52b 13: MI52c

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

(b) SIMS on SIMS Cameca ims-5f

Table 2 Li concentrations and Li isotopic compositions of whole-rock samples Schiavi, Federica et al. (2009)

1: ST103 2: ST79 3: ST81 4: ST82 5: STR317 6: STR010203 7: STR170503

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

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

Table 1S(b). Major element compositions of olivine-hosted melt inclusions from San Bartolo lava Schiavi, Federica et al. (2011)

1: MI2b 2: MI3g 3: MI4d 4: MI8e 5: MI59 6: MI60-1 7: MI60-2 8: MI62 9: MI64 10: MI74

(a) EPMA on EPMA

@article{20180305113432-690138,
 author={{ST103}},
 title={Hand specimen with quantity 89.23 g at \nolinkurl{/ISEI/main/126/A/6/Volcanics from Mt. Etna and Mt. Stromboli/}},
 journal={\href{http://dream.misasa.okayama-u.ac.jp/?q=20180305113432-690138}{DREAM}},
 volume={20},
 pages={20180305113432-690138},
 year={2018},
 url={http://dream.misasa.okayama-u.ac.jp/?q=20180305113432-690138},
}

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<acquisitions>
  <acquisition>
    <global_id>20200225142837-571328</global_id>
    <name>ST103</name>
    <device>Q-ICPMS Agilent 7500cs</device>
    <technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
    <operator>Federica</operator>
    <sample_global_id>20180305113432-690138</sample_global_id>
    <sample_name>ST103</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>8.96</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cr</nickname>
        <value>247.0</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ni</nickname>
        <value>87.4</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Rb</nickname>
        <value>59.9</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sr</nickname>
        <value>515.0</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Y</nickname>
        <value>19.3</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Zr</nickname>
        <value>102.0</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nb</nickname>
        <value>10.9</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Cs</nickname>
        <value>4.33</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ba</nickname>
        <value>728.0</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>La</nickname>
        <value>26.7</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ce</nickname>
        <value>53.7</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pr</nickname>
        <value>6.38</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Nd</nickname>
        <value>25.9</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Sm</nickname>
        <value>5.14</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Eu</nickname>
        <value>1.38</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Gd</nickname>
        <value>5.07</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tb</nickname>
        <value>0.686</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Dy</nickname>
        <value>3.94</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Ho</nickname>
        <value>0.775</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Er</nickname>
        <value>2.16</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Tm</nickname>
        <value>0.304</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Yb</nickname>
        <value>2.03</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Lu</nickname>
        <value>0.308</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Pb</nickname>
        <value>14.1</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Th</nickname>
        <value>11.3</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>U</nickname>
        <value>3.05</value>
        <unit>ug/g</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20200225155344-329300</global_id>
    <name>ST103</name>
    <device>EPMA</device>
    <technique>EPMA</technique>
    <operator>Federica</operator>
    <sample_global_id>20180305113432-690138</sample_global_id>
    <sample_name>ST103</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>SiO2</nickname>
        <value>52.32</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>TiO2</nickname>
        <value>0.77</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Al2O3</nickname>
        <value>17.03</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Fe2O3</nickname>
        <value>8.08</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MnO</nickname>
        <value>0.15</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>MgO</nickname>
        <value>7.0</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>CaO</nickname>
        <value>10.95</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>Na2O</nickname>
        <value>2.34</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>K2O</nickname>
        <value>1.8</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>P2O5</nickname>
        <value>0.27</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>LOI</nickname>
        <value>-0.23</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
      <analysis>
        <nickname>total</nickname>
        <value>100.48</value>
        <unit>%</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20200410122516-270319</global_id>
    <name>ST103</name>
    <device>Q-ICPMS Agilent 7500cs</device>
    <technique>Q-ICP-MS_procedures of Makishima and Nakamura (1997, 1999, 2006)</technique>
    <operator>Federica</operator>
    <sample_global_id>20180305113432-690138</sample_global_id>
    <sample_name>ST103</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>Li</nickname>
        <value>8.59</value>
        <unit>ppm</unit>
        <uncertainty/>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
  <acquisition>
    <global_id>20200410122525-942456</global_id>
    <name>ST103</name>
    <device>MC-ICP-MS Finnigan, Neptune</device>
    <technique>Li isotopes_procedures of Moriguti and Nakamura (1998)</technique>
    <operator>Federica</operator>
    <sample_global_id>20180305113432-690138</sample_global_id>
    <sample_name>ST103</sample_name>
    <description/>
    <chemistries>
      <analysis>
        <nickname>d7Li</nickname>
        <value>3.12</value>
        <unit>permil</unit>
        <uncertainty>0.03</uncertainty>
        <label/>
        <info/>
      </analysis>
    </chemistries>
  </acquisition>
</acquisitions>

name

physical-form

quantity

ol2b pub

grain

20200225152740-421375

ol3g pub

grain

20200225152810-964556

ol4d pub

grain

20200225152922-267178

ol59 pub

grain

20200225153106-388905

ol60-1 pub

grain

20200225153106-868826

ol60-2 pub

grain

20200225153323-657907

ol62 pub

grain

20200225153106-584044

ol64 pub

grain

20200225153425-730174

ol74 pub

grain

20200225153425-597697

ol8e pub

grain

20200225153001-677257

place quantity

ISEI/main/126/A/6/Volcanics from Mt. Etna and Mt. Stromboli about 1 month

2020-04-10 14:37 2020-05-16 11:57

description:

ISEI/main/126/Volcanics from Mt. Etna and Mt. Stromboli about 2 years

2018-03-05 11:34 2020-04-10 14:37

description:

name	device	global-id
MI62 pub 2 on MI62 pub	SIMS Cameca ims-1270	20200225151508-898410
MI2b pub 3 on MI2b pub	SIMS Cameca ims-1270	20200225151508-768192
MI3g pub 2 on MI3g pub	SIMS Cameca ims-1270	20200225151508-496637
MI60-1 pub 3 on MI60-1 pub	SIMS Cameca ims-1270	20200225151508-583176
MI4d pub 3 on MI4d pub	SIMS Cameca ims-1270	20200225151508-978799
MI59 pub 2 on MI59 pub	SIMS Cameca ims-1270	20200225151508-533382
ST103 pub 27	Q-ICPMS Agilent 7500cs	20200225142837-571328
MI60-1 pub 17 on MI60-1 pub	SIMS Cameca ims-5f	20200225145727-679164
MI60-2 pub 31 on MI60-2 pub	SIMS Cameca ims-5f	20200225145727-996191
MI2b pub 31 on MI2b pub	SIMS Cameca ims-5f	20200225144653-629927
MI3g pub 31 on MI3g pub	SIMS Cameca ims-5f	20200225144653-134856
MI4d pub 32 on MI4d pub	SIMS Cameca ims-5f	20200225144654-371170
MI8e pub 31 on MI8e pub	SIMS Cameca ims-5f	20200225144655-377540
MI60-1 pub 13 on MI60-1 pub	EPMA	20200225155346-343967
ol60-2 pub 7 on ol60-2 pub	SEM-EDX 3100H with HORIBA EMAX	20200226095341-430996
MI60-2 pub 10 on MI60-2 pub	EPMA	20200225155346-572295
MI2b pub 13 on MI2b pub	EPMA	20200225155344-815820
ol2b pub 7 on ol2b pub	SEM-EDX 3100H with HORIBA EMAX	20200226095338-912494
ol62 pub 7 on ol62 pub	SEM-EDX 3100H with HORIBA EMAX	20200226095341-342362
MI3g pub 10 on MI3g pub	EPMA	20200225155345-499424
MI62 pub 13 on MI62 pub	EPMA	20200225155347-337564
ol3g pub 7 on ol3g pub	SEM-EDX 3100H with HORIBA EMAX	20200226095338-687797
MI4d pub 13 on MI4d pub	EPMA	20200225155345-976718
MI64 pub 10 on MI64 pub	EPMA	20200225155347-463278
ol64 pub 7 on ol64 pub	SEM-EDX 3100H with HORIBA EMAX	20200226095341-100550
ol4d pub 7 on ol4d pub	SEM-EDX 3100H with HORIBA EMAX	20200226095338-558615
MI8e pub 10 on MI8e pub	EPMA	20200225155345-444446
MI74 pub 13 on MI74 pub	EPMA	20200225155347-533678
MI159 pub 12 on MI59 pub	EPMA	20200225155346-186926
ol74 pub 7 on ol74 pub	SEM-EDX 3100H with HORIBA EMAX	20200226095341-462944
ol8e pub 7 on ol8e pub	SEM-EDX 3100H with HORIBA EMAX	20200226095339-949854
ST103 pub 12	EPMA	20200225155344-329300
ol59 pub 7 on ol59 pub	SEM-EDX 3100H with HORIBA EMAX	20200226095339-393270
ol60-1 pub 7 on ol60-1 pub	SEM-EDX 3100H with HORIBA EMAX	20200226095339-642242
ST103 pub 1	Q-ICPMS Agilent 7500cs	20200410122516-270319
ST103 pub 1	MC-ICP-MS Finnigan, Neptune	20200410122525-942456

	name		global-id
	Schiavi, Federica (2009) Degassing, crystallization and eruption dynamics at Stromboli: trace element and lithium isotopic evidence from 2003 ashes, Contributions to Mineralogy and Petrology, 159, 541-561. Table 2 Li concentrations and Li isotopic compositions of whole-rock samples		20100403102859038.admin
	Schiavi, Federica (2011) Trace element and Pb–B–Li isotope systematics of olivine-hosted melt inclusions: insights into source metasomatism beneath Stromboli (southern Italy), Contributions to Mineralogy and Petrology, 163. Table 1S. Major element compositions of San Bartolo lava Table 1S(a). Major element compositions of olivine grains from San Bartolo lava Table 1 Trace element composition of San Bartolo lava and olivine-hosted melt inclusions Table 1S(b). Major element compositions of olivine-hosted melt inclusions from San Bartolo lava Table 2 Pb, B and Li isotopic compositions of olivine-hosted melt inclusions		20200225102214-755085

		name		spots	global-id
		tixhr1325357757.jpg pub		0	20180305113437-451599