Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan
Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are t...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yuji ichiyama [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2017 |
|---|
| Schlagwörter: |
|---|
| Übergeordnetes Werk: |
Enthalten in: American mineralogist - Washington, DC [u.a.] : Soc., 1916, 102(2017), 2, Seite 341-346 |
|---|---|
| Übergeordnetes Werk: |
volume:102 ; year:2017 ; number:2 ; pages:341-346 |
| Links: |
|---|
| DOI / URN: |
10.2138/am-2017-5720 |
|---|
| Katalog-ID: |
OLC199095488X |
|---|
| LEADER | 01000caa a2200265 4500 | ||
|---|---|---|---|
| 001 | OLC199095488X | ||
| 003 | DE-627 | ||
| 005 | 20230514041541.0 | ||
| 007 | tu | ||
| 008 | 170303s2017 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.2138/am-2017-5720 |2 doi | |
| 028 | 5 | 2 | |a PQ20170301 |
| 035 | |a (DE-627)OLC199095488X | ||
| 035 | |a (DE-599)GBVOLC199095488X | ||
| 035 | |a (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 | ||
| 035 | |a (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |a 540 |q DNB |
| 084 | |a 38.30 |2 bkl | ||
| 100 | 0 | |a Yuji ichiyama |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan |
| 264 | 1 | |c 2017 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 520 | |a Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. | ||
| 650 | 4 | |a Sea of Japan | |
| 650 | 4 | |a Mantle xenolith | |
| 650 | 4 | |a secondary orthopyroxene | |
| 650 | 4 | |a adakite | |
| 700 | 0 | |a Tomoaki morishita |4 oth | |
| 700 | 0 | |a Akihiro Tamura |4 oth | |
| 700 | 0 | |a Shoji Arai |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |t American mineralogist |d Washington, DC [u.a.] : Soc., 1916 |g 102(2017), 2, Seite 341-346 |w (DE-627)129081795 |w (DE-600)3514-2 |w (DE-576)014414716 |x 0003-004X |7 nnns |
| 773 | 1 | 8 | |g volume:102 |g year:2017 |g number:2 |g pages:341-346 |
| 856 | 4 | 1 | |u http://dx.doi.org/10.2138/am-2017-5720 |3 Volltext |
| 856 | 4 | 2 | |u http://www.degruyter.com/doi/10.2138/am-2017-5720 |
| 856 | 4 | 2 | |u http://search.proquest.com/docview/1871606532 |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-CHE | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a SSG-OLC-DE-84 | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_21 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_65 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_188 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2015 | ||
| 912 | |a GBV_ILN_4012 | ||
| 912 | |a GBV_ILN_4112 | ||
| 912 | |a GBV_ILN_4323 | ||
| 936 | b | k | |a 38.30 |q AVZ |
| 951 | |a AR | ||
| 952 | |d 102 |j 2017 |e 2 |h 341-346 | ||
| author_variant |
y i yi |
|---|---|
| matchkey_str |
article:0003004X:2017----::dktmtsmtsiaakrmnlprdttxnl |
| hierarchy_sort_str |
2017 |
| bklnumber |
38.30 |
| publishDate |
2017 |
| allfields |
10.2138/am-2017-5720 doi PQ20170301 (DE-627)OLC199095488X (DE-599)GBVOLC199095488X (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol DE-627 ger DE-627 rakwb eng 550 540 DNB 38.30 bkl Yuji ichiyama verfasserin aut Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. Sea of Japan Mantle xenolith secondary orthopyroxene adakite Tomoaki morishita oth Akihiro Tamura oth Shoji Arai oth Enthalten in American mineralogist Washington, DC [u.a.] : Soc., 1916 102(2017), 2, Seite 341-346 (DE-627)129081795 (DE-600)3514-2 (DE-576)014414716 0003-004X nnns volume:102 year:2017 number:2 pages:341-346 http://dx.doi.org/10.2138/am-2017-5720 Volltext http://www.degruyter.com/doi/10.2138/am-2017-5720 http://search.proquest.com/docview/1871606532 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4323 38.30 AVZ AR 102 2017 2 341-346 |
| spelling |
10.2138/am-2017-5720 doi PQ20170301 (DE-627)OLC199095488X (DE-599)GBVOLC199095488X (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol DE-627 ger DE-627 rakwb eng 550 540 DNB 38.30 bkl Yuji ichiyama verfasserin aut Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. Sea of Japan Mantle xenolith secondary orthopyroxene adakite Tomoaki morishita oth Akihiro Tamura oth Shoji Arai oth Enthalten in American mineralogist Washington, DC [u.a.] : Soc., 1916 102(2017), 2, Seite 341-346 (DE-627)129081795 (DE-600)3514-2 (DE-576)014414716 0003-004X nnns volume:102 year:2017 number:2 pages:341-346 http://dx.doi.org/10.2138/am-2017-5720 Volltext http://www.degruyter.com/doi/10.2138/am-2017-5720 http://search.proquest.com/docview/1871606532 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4323 38.30 AVZ AR 102 2017 2 341-346 |
| allfields_unstemmed |
10.2138/am-2017-5720 doi PQ20170301 (DE-627)OLC199095488X (DE-599)GBVOLC199095488X (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol DE-627 ger DE-627 rakwb eng 550 540 DNB 38.30 bkl Yuji ichiyama verfasserin aut Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. Sea of Japan Mantle xenolith secondary orthopyroxene adakite Tomoaki morishita oth Akihiro Tamura oth Shoji Arai oth Enthalten in American mineralogist Washington, DC [u.a.] : Soc., 1916 102(2017), 2, Seite 341-346 (DE-627)129081795 (DE-600)3514-2 (DE-576)014414716 0003-004X nnns volume:102 year:2017 number:2 pages:341-346 http://dx.doi.org/10.2138/am-2017-5720 Volltext http://www.degruyter.com/doi/10.2138/am-2017-5720 http://search.proquest.com/docview/1871606532 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4323 38.30 AVZ AR 102 2017 2 341-346 |
| allfieldsGer |
10.2138/am-2017-5720 doi PQ20170301 (DE-627)OLC199095488X (DE-599)GBVOLC199095488X (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol DE-627 ger DE-627 rakwb eng 550 540 DNB 38.30 bkl Yuji ichiyama verfasserin aut Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. Sea of Japan Mantle xenolith secondary orthopyroxene adakite Tomoaki morishita oth Akihiro Tamura oth Shoji Arai oth Enthalten in American mineralogist Washington, DC [u.a.] : Soc., 1916 102(2017), 2, Seite 341-346 (DE-627)129081795 (DE-600)3514-2 (DE-576)014414716 0003-004X nnns volume:102 year:2017 number:2 pages:341-346 http://dx.doi.org/10.2138/am-2017-5720 Volltext http://www.degruyter.com/doi/10.2138/am-2017-5720 http://search.proquest.com/docview/1871606532 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4323 38.30 AVZ AR 102 2017 2 341-346 |
| allfieldsSound |
10.2138/am-2017-5720 doi PQ20170301 (DE-627)OLC199095488X (DE-599)GBVOLC199095488X (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol DE-627 ger DE-627 rakwb eng 550 540 DNB 38.30 bkl Yuji ichiyama verfasserin aut Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. Sea of Japan Mantle xenolith secondary orthopyroxene adakite Tomoaki morishita oth Akihiro Tamura oth Shoji Arai oth Enthalten in American mineralogist Washington, DC [u.a.] : Soc., 1916 102(2017), 2, Seite 341-346 (DE-627)129081795 (DE-600)3514-2 (DE-576)014414716 0003-004X nnns volume:102 year:2017 number:2 pages:341-346 http://dx.doi.org/10.2138/am-2017-5720 Volltext http://www.degruyter.com/doi/10.2138/am-2017-5720 http://search.proquest.com/docview/1871606532 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4323 38.30 AVZ AR 102 2017 2 341-346 |
| language |
English |
| source |
Enthalten in American mineralogist 102(2017), 2, Seite 341-346 volume:102 year:2017 number:2 pages:341-346 |
| sourceStr |
Enthalten in American mineralogist 102(2017), 2, Seite 341-346 volume:102 year:2017 number:2 pages:341-346 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Sea of Japan Mantle xenolith secondary orthopyroxene adakite |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
American mineralogist |
| authorswithroles_txt_mv |
Yuji ichiyama @@aut@@ Tomoaki morishita @@oth@@ Akihiro Tamura @@oth@@ Shoji Arai @@oth@@ |
| publishDateDaySort_date |
2017-01-01T00:00:00Z |
| hierarchy_top_id |
129081795 |
| dewey-sort |
3550 |
| id |
OLC199095488X |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC199095488X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230514041541.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">170303s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.2138/am-2017-5720</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20170301</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC199095488X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC199095488X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="a">540</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.30</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Yuji ichiyama</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea of Japan</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mantle xenolith</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">secondary orthopyroxene</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">adakite</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Tomoaki morishita</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Akihiro Tamura</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Shoji Arai</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">American mineralogist</subfield><subfield code="d">Washington, DC [u.a.] : Soc., 1916</subfield><subfield code="g">102(2017), 2, Seite 341-346</subfield><subfield code="w">(DE-627)129081795</subfield><subfield code="w">(DE-600)3514-2</subfield><subfield code="w">(DE-576)014414716</subfield><subfield code="x">0003-004X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:102</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:2</subfield><subfield code="g">pages:341-346</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.2138/am-2017-5720</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.degruyter.com/doi/10.2138/am-2017-5720</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1871606532</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.30</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">102</subfield><subfield code="j">2017</subfield><subfield code="e">2</subfield><subfield code="h">341-346</subfield></datafield></record></collection>
|
| author |
Yuji ichiyama |
| spellingShingle |
Yuji ichiyama ddc 550 bkl 38.30 misc Sea of Japan misc Mantle xenolith misc secondary orthopyroxene misc adakite Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan |
| authorStr |
Yuji ichiyama |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)129081795 |
| format |
Article |
| dewey-ones |
550 - Earth sciences 540 - Chemistry & allied sciences |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0003-004X |
| topic_title |
550 540 DNB 38.30 bkl Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan Sea of Japan Mantle xenolith secondary orthopyroxene adakite |
| topic |
ddc 550 bkl 38.30 misc Sea of Japan misc Mantle xenolith misc secondary orthopyroxene misc adakite |
| topic_unstemmed |
ddc 550 bkl 38.30 misc Sea of Japan misc Mantle xenolith misc secondary orthopyroxene misc adakite |
| topic_browse |
ddc 550 bkl 38.30 misc Sea of Japan misc Mantle xenolith misc secondary orthopyroxene misc adakite |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| author2_variant |
t m tm a t at s a sa |
| hierarchy_parent_title |
American mineralogist |
| hierarchy_parent_id |
129081795 |
| dewey-tens |
550 - Earth sciences & geology 540 - Chemistry |
| hierarchy_top_title |
American mineralogist |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)129081795 (DE-600)3514-2 (DE-576)014414716 |
| title |
Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan |
| ctrlnum |
(DE-627)OLC199095488X (DE-599)GBVOLC199095488X (PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170 (KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol |
| title_full |
Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan |
| author_sort |
Yuji ichiyama |
| journal |
American mineralogist |
| journalStr |
American mineralogist |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2017 |
| contenttype_str_mv |
txt |
| container_start_page |
341 |
| author_browse |
Yuji ichiyama |
| container_volume |
102 |
| class |
550 540 DNB 38.30 bkl |
| format_se |
Aufsätze |
| author-letter |
Yuji ichiyama |
| doi_str_mv |
10.2138/am-2017-5720 |
| dewey-full |
550 540 |
| title_sort |
adakite metasomatism in a back-arc mantle peridotite xenolith from the sea of japan |
| title_auth |
Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan |
| abstract |
Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. |
| abstractGer |
Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. |
| abstract_unstemmed |
Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins. |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO GBV_ILN_21 GBV_ILN_22 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_188 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4112 GBV_ILN_4323 |
| container_issue |
2 |
| title_short |
Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan |
| url |
http://dx.doi.org/10.2138/am-2017-5720 http://www.degruyter.com/doi/10.2138/am-2017-5720 http://search.proquest.com/docview/1871606532 |
| remote_bool |
false |
| author2 |
Tomoaki morishita Akihiro Tamura Shoji Arai |
| author2Str |
Tomoaki morishita Akihiro Tamura Shoji Arai |
| ppnlink |
129081795 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth oth oth |
| doi_str |
10.2138/am-2017-5720 |
| up_date |
2024-07-04T02:16:36.617Z |
| _version_ |
1803613001869164544 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a2200265 4500</leader><controlfield tag="001">OLC199095488X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230514041541.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">170303s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.2138/am-2017-5720</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">PQ20170301</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC199095488X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)GBVOLC199095488X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(PRQ)p801-b32c5d5b87640706972262d46a793b1328250bea4b06033e1cd3ee5230ba6c170</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(KEY)0120180820170000102000200341adakitemetasomatisminabackarcmantleperidotitexenol</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="a">540</subfield><subfield code="q">DNB</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.30</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">Yuji ichiyama</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Adakite metasomatism in a back-arc mantle peridotite xenolith from the Sea of Japan</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Secondary orthopyroxenes occur as veinlets (<0.1 mm thick) cutting an olivine grain in a two-pyroxene peridotite xenolith from the Shiribeshi Seamount in the Sea of Japan. These orthopyroxenes are characterized by low Al (0.4–1.7 wt%), Cr (<0.1 wt%), and CaO (0.3–0.4 wt%) contents, which are the same signatures of the secondary orthopyroxenes in peridotite xenoliths from island arcs. The trace-element patterns of the melts in equilibrium with the secondary orthopyroxenes show enrichment in light rare earth elements and Sr and depletion in heavy rare earth elements, Nb and Ti. These trace-element characteristics are highly consistent with those of slab-derived adakites. The involvement of slab-derived melts in the mantle beneath the Sea of Japan has been inferred from the geochemical characteristics of the volcanic rocks formed during opening of the Sea of Japan. The source mantle of the enriched basalts in the Sea of Japan is likely to have been metasomatized by adakitic melts in the same manner as the peridotite-hosted veinlet. The secondary orthopyroxenes in the peridotite xenolith from the Shiribeshi Seamount provide direct evidence for the metasomatic infux of adakitic melts into the back-arc mantle beneath the Sea of Japan. Adakitic metasomatism, as documented in the Sea of Japan, potentially plays an important role in mantle evolution and magma generation beneath global back-arc basins.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea of Japan</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mantle xenolith</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">secondary orthopyroxene</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">adakite</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Tomoaki morishita</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Akihiro Tamura</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Shoji Arai</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">American mineralogist</subfield><subfield code="d">Washington, DC [u.a.] : Soc., 1916</subfield><subfield code="g">102(2017), 2, Seite 341-346</subfield><subfield code="w">(DE-627)129081795</subfield><subfield code="w">(DE-600)3514-2</subfield><subfield code="w">(DE-576)014414716</subfield><subfield code="x">0003-004X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:102</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:2</subfield><subfield code="g">pages:341-346</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">http://dx.doi.org/10.2138/am-2017-5720</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://www.degruyter.com/doi/10.2138/am-2017-5720</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">http://search.proquest.com/docview/1871606532</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.30</subfield><subfield code="q">AVZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">102</subfield><subfield code="j">2017</subfield><subfield code="e">2</subfield><subfield code="h">341-346</subfield></datafield></record></collection>
|
| score |
7.400305 |