The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan

Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral p...
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Autor*in:	Ikehata, Kei [verfasserIn] Yasuda, Atsushi [verfasserIn] Notsu, Kenji [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2009

Schlagwörter:	Olivine Olivine Crystal Olivine Phenocryst Scoria Sample Sulfide Saturation

Übergeordnetes Werk:	Enthalten in: Mineralogy and petrology - Wien [u.a.] : Springer, 1948, 99(2009), 1-2 vom: 23. Okt., Seite 143-152
Übergeordnetes Werk:	volume:99 ; year:2009 ; number:1-2 ; day:23 ; month:10 ; pages:143-152

Links:	Volltext

DOI / URN:	10.1007/s00710-009-0086-x

Katalog-ID:	SPR007562888

Internformat


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245	1	4	\|a The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan
264		1	\|c 2009
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520			\|a Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion.
650		4	\|a Olivine \|7 (dpeaa)DE-He213
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650		4	\|a Olivine Phenocryst \|7 (dpeaa)DE-He213
650		4	\|a Scoria Sample \|7 (dpeaa)DE-He213
650		4	\|a Sulfide Saturation \|7 (dpeaa)DE-He213
700	1		\|a Yasuda, Atsushi \|e verfasserin \|4 aut
700	1		\|a Notsu, Kenji \|e verfasserin \|4 aut
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936	b	k	\|a 38.25 \|q ASE
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951			\|a AR
952			\|d 99 \|j 2009 \|e 1-2 \|b 23 \|c 10 \|h 143-152

Indexfelder

author_variant	k i ki a y ay k n kn
matchkey_str	article:14381168:2009----::hgohmsrovltlseisnetnlsosnslieieas
hierarchy_sort_str	2009
bklnumber	38.25 38.30
publishDate	2009
allfields	10.1007/s00710-009-0086-x doi (DE-627)SPR007562888 (SPR)s00710-009-0086-x-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.30 bkl Ikehata, Kei verfasserin aut The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion. Olivine (dpeaa)DE-He213 Olivine Crystal (dpeaa)DE-He213 Olivine Phenocryst (dpeaa)DE-He213 Scoria Sample (dpeaa)DE-He213 Sulfide Saturation (dpeaa)DE-He213 Yasuda, Atsushi verfasserin aut Notsu, Kenji verfasserin aut Enthalten in Mineralogy and petrology Wien [u.a.] : Springer, 1948 99(2009), 1-2 vom: 23. Okt., Seite 143-152 (DE-627)254637922 (DE-600)1462900-8 1438-1168 nnns volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152 https://dx.doi.org/10.1007/s00710-009-0086-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 ASE 38.30 ASE AR 99 2009 1-2 23 10 143-152
spelling	10.1007/s00710-009-0086-x doi (DE-627)SPR007562888 (SPR)s00710-009-0086-x-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.30 bkl Ikehata, Kei verfasserin aut The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion. Olivine (dpeaa)DE-He213 Olivine Crystal (dpeaa)DE-He213 Olivine Phenocryst (dpeaa)DE-He213 Scoria Sample (dpeaa)DE-He213 Sulfide Saturation (dpeaa)DE-He213 Yasuda, Atsushi verfasserin aut Notsu, Kenji verfasserin aut Enthalten in Mineralogy and petrology Wien [u.a.] : Springer, 1948 99(2009), 1-2 vom: 23. Okt., Seite 143-152 (DE-627)254637922 (DE-600)1462900-8 1438-1168 nnns volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152 https://dx.doi.org/10.1007/s00710-009-0086-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 ASE 38.30 ASE AR 99 2009 1-2 23 10 143-152
allfields_unstemmed	10.1007/s00710-009-0086-x doi (DE-627)SPR007562888 (SPR)s00710-009-0086-x-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.30 bkl Ikehata, Kei verfasserin aut The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion. Olivine (dpeaa)DE-He213 Olivine Crystal (dpeaa)DE-He213 Olivine Phenocryst (dpeaa)DE-He213 Scoria Sample (dpeaa)DE-He213 Sulfide Saturation (dpeaa)DE-He213 Yasuda, Atsushi verfasserin aut Notsu, Kenji verfasserin aut Enthalten in Mineralogy and petrology Wien [u.a.] : Springer, 1948 99(2009), 1-2 vom: 23. Okt., Seite 143-152 (DE-627)254637922 (DE-600)1462900-8 1438-1168 nnns volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152 https://dx.doi.org/10.1007/s00710-009-0086-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 ASE 38.30 ASE AR 99 2009 1-2 23 10 143-152
allfieldsGer	10.1007/s00710-009-0086-x doi (DE-627)SPR007562888 (SPR)s00710-009-0086-x-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.30 bkl Ikehata, Kei verfasserin aut The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion. Olivine (dpeaa)DE-He213 Olivine Crystal (dpeaa)DE-He213 Olivine Phenocryst (dpeaa)DE-He213 Scoria Sample (dpeaa)DE-He213 Sulfide Saturation (dpeaa)DE-He213 Yasuda, Atsushi verfasserin aut Notsu, Kenji verfasserin aut Enthalten in Mineralogy and petrology Wien [u.a.] : Springer, 1948 99(2009), 1-2 vom: 23. Okt., Seite 143-152 (DE-627)254637922 (DE-600)1462900-8 1438-1168 nnns volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152 https://dx.doi.org/10.1007/s00710-009-0086-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 ASE 38.30 ASE AR 99 2009 1-2 23 10 143-152
allfieldsSound	10.1007/s00710-009-0086-x doi (DE-627)SPR007562888 (SPR)s00710-009-0086-x-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.30 bkl Ikehata, Kei verfasserin aut The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion. Olivine (dpeaa)DE-He213 Olivine Crystal (dpeaa)DE-He213 Olivine Phenocryst (dpeaa)DE-He213 Scoria Sample (dpeaa)DE-He213 Sulfide Saturation (dpeaa)DE-He213 Yasuda, Atsushi verfasserin aut Notsu, Kenji verfasserin aut Enthalten in Mineralogy and petrology Wien [u.a.] : Springer, 1948 99(2009), 1-2 vom: 23. Okt., Seite 143-152 (DE-627)254637922 (DE-600)1462900-8 1438-1168 nnns volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152 https://dx.doi.org/10.1007/s00710-009-0086-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_206 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.25 ASE 38.30 ASE AR 99 2009 1-2 23 10 143-152
language	English
source	Enthalten in Mineralogy and petrology 99(2009), 1-2 vom: 23. Okt., Seite 143-152 volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152
sourceStr	Enthalten in Mineralogy and petrology 99(2009), 1-2 vom: 23. Okt., Seite 143-152 volume:99 year:2009 number:1-2 day:23 month:10 pages:143-152
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Olivine Olivine Crystal Olivine Phenocryst Scoria Sample Sulfide Saturation
dewey-raw	550
isfreeaccess_bool	false
container_title	Mineralogy and petrology
authorswithroles_txt_mv	Ikehata, Kei @@aut@@ Yasuda, Atsushi @@aut@@ Notsu, Kenji @@aut@@
publishDateDaySort_date	2009-10-23T00:00:00Z
hierarchy_top_id	254637922
dewey-sort	3550
id	SPR007562888
language_de	englisch
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author	Ikehata, Kei
spellingShingle	Ikehata, Kei ddc 550 bkl 38.25 bkl 38.30 misc Olivine misc Olivine Crystal misc Olivine Phenocryst misc Scoria Sample misc Sulfide Saturation The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan
authorStr	Ikehata, Kei
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topic_title	550 ASE 38.25 bkl 38.30 bkl The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan Olivine (dpeaa)DE-He213 Olivine Crystal (dpeaa)DE-He213 Olivine Phenocryst (dpeaa)DE-He213 Scoria Sample (dpeaa)DE-He213 Sulfide Saturation (dpeaa)DE-He213
topic	ddc 550 bkl 38.25 bkl 38.30 misc Olivine misc Olivine Crystal misc Olivine Phenocryst misc Scoria Sample misc Sulfide Saturation
topic_unstemmed	ddc 550 bkl 38.25 bkl 38.30 misc Olivine misc Olivine Crystal misc Olivine Phenocryst misc Scoria Sample misc Sulfide Saturation
topic_browse	ddc 550 bkl 38.25 bkl 38.30 misc Olivine misc Olivine Crystal misc Olivine Phenocryst misc Scoria Sample misc Sulfide Saturation
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title	The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan
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title_full	The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan
author_sort	Ikehata, Kei
journal	Mineralogy and petrology
journalStr	Mineralogy and petrology
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author_browse	Ikehata, Kei Yasuda, Atsushi Notsu, Kenji
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author-letter	Ikehata, Kei
doi_str_mv	10.1007/s00710-009-0086-x
dewey-full	550
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title_sort	geochemistry of volatile species in melt inclusions and sulfide minerals from izu-oshima volcano, japan
title_auth	The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan
abstract	Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion.
abstractGer	Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion.
abstract_unstemmed	Abstract Olivine-hosted melt inclusions in the O95 pyroclastic layer of Izu-Oshima volcano, Japan are basaltic to basaltic-andesitic in composition. The negative correlation between $ SiO_{2} $ and $ H_{2} $O in melt inclusions and reverse compositional zoning observed in olivine and other mineral phenocrysts is inferred to arise from mixing between a highly evolved and a less evolved magma. The latter is characterized by the highest S (0.15 wt.%) and $ H_{2} $O (3.4 wt.%) concentrations among those described in reports of previous studies. The $ S^{6+} $/$ S_{total} $ ratios in melt inclusions were 0.64 – 0.73, suggesting a relatively high oxidation state (NNO + 0.87 at 1150°C). The presence of pyrrhotites, which are found only in titanomagnetite microlites, suggests that sulfide saturation occurred during microlite growth under at a sulfur fugacity (log $ fS_{2} $) value of around + 0.5 for T = 1060°C. The groundmass glass compositions are more evolved (andesitic composition) than any melt inclusions containing high amounts of Cl (0.13 wt.%) but negligible $ H_{2} $O (0.20 wt.%) and S (< 70 ppm), suggesting that Cl was retained in the magma, in contrast to S and $ H_{2} $O, which degassed strongly during magma effusion.
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container_issue	1-2
title_short	The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan
url	https://dx.doi.org/10.1007/s00710-009-0086-x
remote_bool	true
author2	Yasuda, Atsushi Notsu, Kenji
author2Str	Yasuda, Atsushi Notsu, Kenji
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doi_str	10.1007/s00710-009-0086-x
up_date	2024-07-03T13:44:56.570Z
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The geochemistry of volatile species in melt inclusions and sulfide minerals from Izu-Oshima volcano, Japan

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