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Release of mantle helium from forearc region of the Southwest Japan arc
Shikoku, Japan, is an island located on the forearc region of the western sector of the Southwest (SW) Japan arc that was formed by subduction of the Philippine Sea plate beneath the Eurasian plate. Noble gas isotope analyses were carried out for 30 bubbling gas samples and spring water samples coll...
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Published in: | Chemical geology 2006-10, Vol.233 (3), p.235-248 |
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creator | Doğan, Turhan Sumino, Hirochika Nagao, Keisuke Notsu, Kenji |
description | Shikoku, Japan, is an island located on the forearc region of the western sector of the Southwest (SW) Japan arc that was formed by subduction of the Philippine Sea plate beneath the Eurasian plate. Noble gas isotope analyses were carried out for 30 bubbling gas samples and spring water samples collected in Shikoku. In addition, chemical and carbon isotope analyses were conducted for six gas samples. Observed
3He/
4He ratios were 0.17
R/R
A to 3.56
R/R
A, showing that several samples contain mantle helium components, although some samples contain helium of crustal origin. Geographical distributions of
3He/
4He ratios show that high
3He/
4He ratios originate mainly from two areas: one along the Median Tectonic Line (MTL), a major active fault in Japan; the other coinciding with a region in which non-volcanic long-period tremors occur, about 30 km deep [Obara, K., 2002. Nonvolcanic deep tremor associated with subduction in southwest Japan. Science 296, 1679-1681]. This fact indicates that fluids liberated from the slab in the forearc region cause deep tremors and fracturing within the crust, thereby easing the transfer of fluids to the surface that are mixed with mantle helium to the surface. An active fault system can also provide an efficient path for mantle helium transfer. |
doi_str_mv | 10.1016/j.chemgeo.2006.03.008 |
format | article |
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3He/
4He ratios were 0.17
R/R
A to 3.56
R/R
A, showing that several samples contain mantle helium components, although some samples contain helium of crustal origin. Geographical distributions of
3He/
4He ratios show that high
3He/
4He ratios originate mainly from two areas: one along the Median Tectonic Line (MTL), a major active fault in Japan; the other coinciding with a region in which non-volcanic long-period tremors occur, about 30 km deep [Obara, K., 2002. Nonvolcanic deep tremor associated with subduction in southwest Japan. Science 296, 1679-1681]. This fact indicates that fluids liberated from the slab in the forearc region cause deep tremors and fracturing within the crust, thereby easing the transfer of fluids to the surface that are mixed with mantle helium to the surface. An active fault system can also provide an efficient path for mantle helium transfer.</description><identifier>ISSN: 0009-2541</identifier><identifier>EISSN: 1872-6836</identifier><identifier>DOI: 10.1016/j.chemgeo.2006.03.008</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Deep tremor ; Forearc region ; Helium isotopes ; Median Tectonic Line ; Slab-derived fluids ; SW Japan arc</subject><ispartof>Chemical geology, 2006-10, Vol.233 (3), p.235-248</ispartof><rights>2006 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a429t-1dee658977626be0246b9dc1a13a3d279cad4baec999be7cfb55dffba9607b883</citedby><cites>FETCH-LOGICAL-a429t-1dee658977626be0246b9dc1a13a3d279cad4baec999be7cfb55dffba9607b883</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids></links><search><creatorcontrib>Doğan, Turhan</creatorcontrib><creatorcontrib>Sumino, Hirochika</creatorcontrib><creatorcontrib>Nagao, Keisuke</creatorcontrib><creatorcontrib>Notsu, Kenji</creatorcontrib><title>Release of mantle helium from forearc region of the Southwest Japan arc</title><title>Chemical geology</title><description>Shikoku, Japan, is an island located on the forearc region of the western sector of the Southwest (SW) Japan arc that was formed by subduction of the Philippine Sea plate beneath the Eurasian plate. Noble gas isotope analyses were carried out for 30 bubbling gas samples and spring water samples collected in Shikoku. In addition, chemical and carbon isotope analyses were conducted for six gas samples. Observed
3He/
4He ratios were 0.17
R/R
A to 3.56
R/R
A, showing that several samples contain mantle helium components, although some samples contain helium of crustal origin. Geographical distributions of
3He/
4He ratios show that high
3He/
4He ratios originate mainly from two areas: one along the Median Tectonic Line (MTL), a major active fault in Japan; the other coinciding with a region in which non-volcanic long-period tremors occur, about 30 km deep [Obara, K., 2002. Nonvolcanic deep tremor associated with subduction in southwest Japan. Science 296, 1679-1681]. This fact indicates that fluids liberated from the slab in the forearc region cause deep tremors and fracturing within the crust, thereby easing the transfer of fluids to the surface that are mixed with mantle helium to the surface. An active fault system can also provide an efficient path for mantle helium transfer.</description><subject>Deep tremor</subject><subject>Forearc region</subject><subject>Helium isotopes</subject><subject>Median Tectonic Line</subject><subject>Slab-derived fluids</subject><subject>SW Japan arc</subject><issn>0009-2541</issn><issn>1872-6836</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqFkE1LxDAQhoMouK7-BCEnb61J06TNSWTRVVkQ_DiHNJ1us7TNmrSK_96U3buXGQaed5h5ELqmJKWEittdalrot-DSjBCREpYSUp6gBS2LLBElE6doQQiRScZzeo4uQtjFkTLOF2j9Bh3oANg1uNfD2AFuobNTjxvvYnEetDfYw9a6YYbGFvC7m8b2B8KIX_ReDzgSl-is0V2Aq2Nfos_Hh4_VU7J5XT-v7jeJzjM5JrQGELyURSEyUQHJclHJ2lBNmWZ1Vkij67zSYKSUFRSmqTivm6bSUpCiKku2RDeHvXvvvqZ4guptMNB1egA3BUUlI7xkNIL8ABrvQvDQqL23vfa_ihI1a1M7ddSmZm2KMBW1xdzdIQfxi28LXgVjYTBQWw9mVLWz_2z4A33FeWw</recordid><startdate>20061015</startdate><enddate>20061015</enddate><creator>Doğan, Turhan</creator><creator>Sumino, Hirochika</creator><creator>Nagao, Keisuke</creator><creator>Notsu, Kenji</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20061015</creationdate><title>Release of mantle helium from forearc region of the Southwest Japan arc</title><author>Doğan, Turhan ; Sumino, Hirochika ; Nagao, Keisuke ; Notsu, Kenji</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a429t-1dee658977626be0246b9dc1a13a3d279cad4baec999be7cfb55dffba9607b883</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Deep tremor</topic><topic>Forearc region</topic><topic>Helium isotopes</topic><topic>Median Tectonic Line</topic><topic>Slab-derived fluids</topic><topic>SW Japan arc</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Doğan, Turhan</creatorcontrib><creatorcontrib>Sumino, Hirochika</creatorcontrib><creatorcontrib>Nagao, Keisuke</creatorcontrib><creatorcontrib>Notsu, Kenji</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Chemical geology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Doğan, Turhan</au><au>Sumino, Hirochika</au><au>Nagao, Keisuke</au><au>Notsu, Kenji</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Release of mantle helium from forearc region of the Southwest Japan arc</atitle><jtitle>Chemical geology</jtitle><date>2006-10-15</date><risdate>2006</risdate><volume>233</volume><issue>3</issue><spage>235</spage><epage>248</epage><pages>235-248</pages><issn>0009-2541</issn><eissn>1872-6836</eissn><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><abstract>Shikoku, Japan, is an island located on the forearc region of the western sector of the Southwest (SW) Japan arc that was formed by subduction of the Philippine Sea plate beneath the Eurasian plate. Noble gas isotope analyses were carried out for 30 bubbling gas samples and spring water samples collected in Shikoku. In addition, chemical and carbon isotope analyses were conducted for six gas samples. Observed
3He/
4He ratios were 0.17
R/R
A to 3.56
R/R
A, showing that several samples contain mantle helium components, although some samples contain helium of crustal origin. Geographical distributions of
3He/
4He ratios show that high
3He/
4He ratios originate mainly from two areas: one along the Median Tectonic Line (MTL), a major active fault in Japan; the other coinciding with a region in which non-volcanic long-period tremors occur, about 30 km deep [Obara, K., 2002. Nonvolcanic deep tremor associated with subduction in southwest Japan. Science 296, 1679-1681]. This fact indicates that fluids liberated from the slab in the forearc region cause deep tremors and fracturing within the crust, thereby easing the transfer of fluids to the surface that are mixed with mantle helium to the surface. An active fault system can also provide an efficient path for mantle helium transfer.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.chemgeo.2006.03.008</doi><tpages>14</tpages></addata></record> |
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language | eng |
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source | ScienceDirect Journals |
subjects | Deep tremor Forearc region Helium isotopes Median Tectonic Line Slab-derived fluids SW Japan arc |
title | Release of mantle helium from forearc region of the Southwest Japan arc |
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