Simultaneous boninitic and arc-tholeiitic volcanisms in the Izu forearc region during early arc volcanism, based on ODP Leg 125 Site 786
Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were recovered from Leg 125 Site 786. These rocks were all classified into boninites and associated rocks by Leg 125 Shipboard Scientifi...
Gespeichert in:
| Veröffentlicht in: | Contributions to mineralogy and petrology 2007-05, Vol.153 (5), p.509-531 |
|---|---|
| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 531 |
|---|---|
| container_issue | 5 |
| container_start_page | 509 |
| container_title | Contributions to mineralogy and petrology |
| container_volume | 153 |
| creator | Haraguchi, Satoru Ishii, Teruaki |
| description | Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were recovered from Leg 125 Site 786. These rocks were all classified into boninites and associated rocks by Leg 125 Shipboard Scientific Party, and they concluded that boninitic volcanism had occurred before 40 Ma, and arc tholeiitic volcanism began after 40 Ma. In this study, lava flows and breccias that classified into boninite series are divided into two groups, tholeiite and boninite, based on petrographical and petrological properties. Both series are also distinguished by bulk rock composition. It is considered that the sources of both rock types have similar depleted compositions because of their similar, very low bulk HFSE concentrations. We suggest that boninitic and tholeiitic volcanism occurred closely in time and space, and reflected different temperature and water condition. [PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1007/s00410-006-0164-6 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_208174989</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1249717721</sourcerecordid><originalsourceid>FETCH-LOGICAL-c338t-b3c6e973ee8006de8552ab64c191eef32cff1107446015973f17525321c9ae73</originalsourceid><addsrcrecordid>eNpFkNtKAzEQhoMoWKsP4F3w2tXJZjfZXEo9FQoV2vuQprNtZJtosivoE_jYplbwaph_vjn9hFwyuGEA8jYBVAwKAFEAE1UhjsiIVbwsQAl5TEYAuSqVUqfkLKVXyHmj6hH5Xrjd0PXGYxgSXQXvvOudpcavqYm26LehQ_crfYTOGu_SLlHnab9FOv0aaBsiZpBG3Ljg6XqIzm9olrrP_YD_rmu6MgnXNEPz-xc6ww1lZU0XrkcqG3FOTlrTJbz4i2OyfHxYTp6L2fxpOrmbFZbzpi9W3ApUkiM2-dc1NnVdmpWoLFMMseWlbVvGQFaVAFZnsGWyLmteMqsMSj4mV4exbzG8D5h6_RqG6PNGXULDZKUalSF2gGwMKUVs9Vt0OxM_NQO9t1sf7Nb5BL23Wwv-A9oXcio</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>208174989</pqid></control><display><type>article</type><title>Simultaneous boninitic and arc-tholeiitic volcanisms in the Izu forearc region during early arc volcanism, based on ODP Leg 125 Site 786</title><source>SpringerLink Journals - AutoHoldings</source><creator>Haraguchi, Satoru ; Ishii, Teruaki</creator><creatorcontrib>Haraguchi, Satoru ; Ishii, Teruaki</creatorcontrib><description>Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were recovered from Leg 125 Site 786. These rocks were all classified into boninites and associated rocks by Leg 125 Shipboard Scientific Party, and they concluded that boninitic volcanism had occurred before 40 Ma, and arc tholeiitic volcanism began after 40 Ma. In this study, lava flows and breccias that classified into boninite series are divided into two groups, tholeiite and boninite, based on petrographical and petrological properties. Both series are also distinguished by bulk rock composition. It is considered that the sources of both rock types have similar depleted compositions because of their similar, very low bulk HFSE concentrations. We suggest that boninitic and tholeiitic volcanism occurred closely in time and space, and reflected different temperature and water condition. [PUBLICATION ABSTRACT]</description><identifier>ISSN: 0010-7999</identifier><identifier>EISSN: 1432-0967</identifier><identifier>DOI: 10.1007/s00410-006-0164-6</identifier><identifier>CODEN: CMPEAP</identifier><language>eng</language><publisher>Heidelberg: Springer Nature B.V</publisher><subject>Eocene ; Lava ; Lava flows ; Mineralogy ; Oligocene ; Petrology ; Rocks ; Volcanoes</subject><ispartof>Contributions to mineralogy and petrology, 2007-05, Vol.153 (5), p.509-531</ispartof><rights>Springer-Verlag 2007</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c338t-b3c6e973ee8006de8552ab64c191eef32cff1107446015973f17525321c9ae73</citedby><cites>FETCH-LOGICAL-c338t-b3c6e973ee8006de8552ab64c191eef32cff1107446015973f17525321c9ae73</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Haraguchi, Satoru</creatorcontrib><creatorcontrib>Ishii, Teruaki</creatorcontrib><title>Simultaneous boninitic and arc-tholeiitic volcanisms in the Izu forearc region during early arc volcanism, based on ODP Leg 125 Site 786</title><title>Contributions to mineralogy and petrology</title><description>Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were recovered from Leg 125 Site 786. These rocks were all classified into boninites and associated rocks by Leg 125 Shipboard Scientific Party, and they concluded that boninitic volcanism had occurred before 40 Ma, and arc tholeiitic volcanism began after 40 Ma. In this study, lava flows and breccias that classified into boninite series are divided into two groups, tholeiite and boninite, based on petrographical and petrological properties. Both series are also distinguished by bulk rock composition. It is considered that the sources of both rock types have similar depleted compositions because of their similar, very low bulk HFSE concentrations. We suggest that boninitic and tholeiitic volcanism occurred closely in time and space, and reflected different temperature and water condition. [PUBLICATION ABSTRACT]</description><subject>Eocene</subject><subject>Lava</subject><subject>Lava flows</subject><subject>Mineralogy</subject><subject>Oligocene</subject><subject>Petrology</subject><subject>Rocks</subject><subject>Volcanoes</subject><issn>0010-7999</issn><issn>1432-0967</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNpFkNtKAzEQhoMoWKsP4F3w2tXJZjfZXEo9FQoV2vuQprNtZJtosivoE_jYplbwaph_vjn9hFwyuGEA8jYBVAwKAFEAE1UhjsiIVbwsQAl5TEYAuSqVUqfkLKVXyHmj6hH5Xrjd0PXGYxgSXQXvvOudpcavqYm26LehQ_crfYTOGu_SLlHnab9FOv0aaBsiZpBG3Ljg6XqIzm9olrrP_YD_rmu6MgnXNEPz-xc6ww1lZU0XrkcqG3FOTlrTJbz4i2OyfHxYTp6L2fxpOrmbFZbzpi9W3ApUkiM2-dc1NnVdmpWoLFMMseWlbVvGQFaVAFZnsGWyLmteMqsMSj4mV4exbzG8D5h6_RqG6PNGXULDZKUalSF2gGwMKUVs9Vt0OxM_NQO9t1sf7Nb5BL23Wwv-A9oXcio</recordid><startdate>20070501</startdate><enddate>20070501</enddate><creator>Haraguchi, Satoru</creator><creator>Ishii, Teruaki</creator><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7XB</scope><scope>88I</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>D1I</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KB.</scope><scope>L.G</scope><scope>L6V</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PDBOC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>R05</scope></search><sort><creationdate>20070501</creationdate><title>Simultaneous boninitic and arc-tholeiitic volcanisms in the Izu forearc region during early arc volcanism, based on ODP Leg 125 Site 786</title><author>Haraguchi, Satoru ; Ishii, Teruaki</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c338t-b3c6e973ee8006de8552ab64c191eef32cff1107446015973f17525321c9ae73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Eocene</topic><topic>Lava</topic><topic>Lava flows</topic><topic>Mineralogy</topic><topic>Oligocene</topic><topic>Petrology</topic><topic>Rocks</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Haraguchi, Satoru</creatorcontrib><creatorcontrib>Ishii, Teruaki</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Materials Science Collection</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Materials Science Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Materials Science Collection</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><jtitle>Contributions to mineralogy and petrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Haraguchi, Satoru</au><au>Ishii, Teruaki</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Simultaneous boninitic and arc-tholeiitic volcanisms in the Izu forearc region during early arc volcanism, based on ODP Leg 125 Site 786</atitle><jtitle>Contributions to mineralogy and petrology</jtitle><date>2007-05-01</date><risdate>2007</risdate><volume>153</volume><issue>5</issue><spage>509</spage><epage>531</epage><pages>509-531</pages><issn>0010-7999</issn><eissn>1432-0967</eissn><coden>CMPEAP</coden><abstract>Early arc volcanism during Eocene to Oligocene in the Izu forearc region was investigated during ODP Legs 125 and 126 in 1989, and effusive and intrusive volcanics were recovered from Leg 125 Site 786. These rocks were all classified into boninites and associated rocks by Leg 125 Shipboard Scientific Party, and they concluded that boninitic volcanism had occurred before 40 Ma, and arc tholeiitic volcanism began after 40 Ma. In this study, lava flows and breccias that classified into boninite series are divided into two groups, tholeiite and boninite, based on petrographical and petrological properties. Both series are also distinguished by bulk rock composition. It is considered that the sources of both rock types have similar depleted compositions because of their similar, very low bulk HFSE concentrations. We suggest that boninitic and tholeiitic volcanism occurred closely in time and space, and reflected different temperature and water condition. [PUBLICATION ABSTRACT]</abstract><cop>Heidelberg</cop><pub>Springer Nature B.V</pub><doi>10.1007/s00410-006-0164-6</doi><tpages>23</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0010-7999 |
| ispartof | Contributions to mineralogy and petrology, 2007-05, Vol.153 (5), p.509-531 |
| issn | 0010-7999 1432-0967 |
| language | eng |
| recordid | cdi_proquest_journals_208174989 |
| source | SpringerLink Journals - AutoHoldings |
| subjects | Eocene Lava Lava flows Mineralogy Oligocene Petrology Rocks Volcanoes |
| title | Simultaneous boninitic and arc-tholeiitic volcanisms in the Izu forearc region during early arc volcanism, based on ODP Leg 125 Site 786 |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-28T21%3A04%3A27IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Simultaneous%20boninitic%20and%20arc-tholeiitic%20volcanisms%20in%20the%20Izu%20forearc%20region%20during%20early%20arc%20volcanism,%20based%20on%20ODP%20Leg%20125%20Site%20786&rft.jtitle=Contributions%20to%20mineralogy%20and%20petrology&rft.au=Haraguchi,%20Satoru&rft.date=2007-05-01&rft.volume=153&rft.issue=5&rft.spage=509&rft.epage=531&rft.pages=509-531&rft.issn=0010-7999&rft.eissn=1432-0967&rft.coden=CMPEAP&rft_id=info:doi/10.1007/s00410-006-0164-6&rft_dat=%3Cproquest_cross%3E1249717721%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=208174989&rft_id=info:pmid/&rfr_iscdi=true |