Loading…
Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan
The Nankai hydrate field, Japan, is an example of gas-hydrate deposits associated with an active subduction zone. In order to determine the origin of gas hydrates in this area, 129I/I ratios together with halogen concentrations were measured in a set of pore-water samples collected from two borehole...
Saved in:
Published in: | Geology (Boulder) 2003-06, Vol.31 (6), p.521-524 |
---|---|
Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | |
---|---|
cites | cdi_FETCH-LOGICAL-a378t-9e0d3d60f126eb496169dc8c7ce66500e1cd626cc33b67b536e70cafda0b2403 |
container_end_page | 524 |
container_issue | 6 |
container_start_page | 521 |
container_title | Geology (Boulder) |
container_volume | 31 |
creator | Fehn, Udo Snyder, Glen T Matsumoto, Ryo Muramatsu, Yasuyuki Tomaru, Hitoshi |
description | The Nankai hydrate field, Japan, is an example of gas-hydrate deposits associated with an active subduction zone. In order to determine the origin of gas hydrates in this area, 129I/I ratios together with halogen concentrations were measured in a set of pore-water samples collected from two boreholes in the Nankai hydrate field. Iodine concentrations are between 100 and 230 µM, i.e., strongly enriched compared to seawater, while Cl concentrations were found to be close to that of seawater. Except for one sample, 129I/I ratios are between 180 and 520 × 10-15, giving minimum ages between 24 and 48 Ma. Because these ages are considerably older than present host sediments ( |
doi_str_mv | 10.1130/0091-7613(2003)031<0521:IDOPWA>2.0.CO;2 |
format | article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_19465556</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>347538811</sourcerecordid><originalsourceid>FETCH-LOGICAL-a378t-9e0d3d60f126eb496169dc8c7ce66500e1cd626cc33b67b536e70cafda0b2403</originalsourceid><addsrcrecordid>eNpdkGFr2zAQhkVpYWm6_yD6YWx0Tk-SJdtrGZS0zTLKMmihH4UinRNliZVJDqH_fjYpo_TTHcf7vnf3EHLJYMSYgEuAimWFYuIzBxBfQLBrkJx9m97Ofj_ffOcjGI1nV_yIDFiVi4yrkh-TwX_XB3Ka0gqA5bIoB-RxGpxvkDrT-mZBQ023ISLdmxZjoialYH3XO7r37ZIuTKLLFxe7SaK-oe0S6S_T_DGemojmK_1ptqY5Iye1WSf8-FqH5On-7mn8I3uYTabjm4fMiKJsswrBCaegZlzhPK8UU5WzpS0sKiUBkFmnuLJWiLkq5lIoLMCa2hmY8xzEkHw6xG5j-LvD1OqNTxbXa9Ng2CXdva-klKoTnr8TrsIuNt1pmgNjZal4nzY5iGwMKUWs9Tb6jYkvmoHuweseoe4R6h687sDrHrw-gNdcgx7PNO-SLg5JCwzJemws7kNcu7dbe38upRDiH6mwh3A</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>201188620</pqid></control><display><type>article</type><title>Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan</title><source>AUTh Library subscriptions: Society of Exploration Geophysicists</source><creator>Fehn, Udo ; Snyder, Glen T ; Matsumoto, Ryo ; Muramatsu, Yasuyuki ; Tomaru, Hitoshi</creator><creatorcontrib>Fehn, Udo ; Snyder, Glen T ; Matsumoto, Ryo ; Muramatsu, Yasuyuki ; Tomaru, Hitoshi</creatorcontrib><description>The Nankai hydrate field, Japan, is an example of gas-hydrate deposits associated with an active subduction zone. In order to determine the origin of gas hydrates in this area, 129I/I ratios together with halogen concentrations were measured in a set of pore-water samples collected from two boreholes in the Nankai hydrate field. Iodine concentrations are between 100 and 230 µM, i.e., strongly enriched compared to seawater, while Cl concentrations were found to be close to that of seawater. Except for one sample, 129I/I ratios are between 180 and 520 × 10-15, giving minimum ages between 24 and 48 Ma. Because these ages are considerably older than present host sediments (<2 Ma) and subducting marine sediments (<21 Ma) in this area, iodine (and, by association, methane in the gas hydrates) must have been derived from source formations located in the continental side of the subduction zone. The results do not support derivation of gas hydrates from present host sediments or currently subducting sediments, but could be related to release and long-time recycling of fluids from marine formations of early Tertiary age.</description><identifier>ISSN: 0091-7613</identifier><identifier>EISSN: 1943-2682</identifier><identifier>DOI: 10.1130/0091-7613(2003)031<0521:IDOPWA>2.0.CO;2</identifier><language>eng</language><publisher>Boulder: Geological Society of America (GSA)</publisher><subject>Asia ; Cenozoic ; Far East ; gas hydrates ; Gases ; geochronology ; Geology ; halogens ; I-129 ; iodine ; isotopes ; Japan ; Leg 131 ; Leg 132 ; Leg 196 ; marine sediments ; mass spectra ; Nankai Trough ; North Pacific ; Northwest Pacific ; Ocean Drilling Program ; Oceanography ; ODP Site 808 ; Pacific Ocean ; pore water ; radioactive isotopes ; relative age ; residence time ; sediments ; spectra ; subduction zones ; Tertiary ; Water ; West Pacific</subject><ispartof>Geology (Boulder), 2003-06, Vol.31 (6), p.521-524</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data supplied by the Geological Society of America @Boulder, CO @USA @United States</rights><rights>Copyright Geological Society of America Jun 2003</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a378t-9e0d3d60f126eb496169dc8c7ce66500e1cd626cc33b67b536e70cafda0b2403</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://pubs.geoscienceworld.org/lithosphere/article-lookup?doi=10.1130/0091-7613(2003)031<0521:IDOPWA>2.0.CO;2$$EHTML$$P50$$Ggeoscienceworld$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,38880,77595</link.rule.ids></links><search><creatorcontrib>Fehn, Udo</creatorcontrib><creatorcontrib>Snyder, Glen T</creatorcontrib><creatorcontrib>Matsumoto, Ryo</creatorcontrib><creatorcontrib>Muramatsu, Yasuyuki</creatorcontrib><creatorcontrib>Tomaru, Hitoshi</creatorcontrib><title>Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan</title><title>Geology (Boulder)</title><description>The Nankai hydrate field, Japan, is an example of gas-hydrate deposits associated with an active subduction zone. In order to determine the origin of gas hydrates in this area, 129I/I ratios together with halogen concentrations were measured in a set of pore-water samples collected from two boreholes in the Nankai hydrate field. Iodine concentrations are between 100 and 230 µM, i.e., strongly enriched compared to seawater, while Cl concentrations were found to be close to that of seawater. Except for one sample, 129I/I ratios are between 180 and 520 × 10-15, giving minimum ages between 24 and 48 Ma. Because these ages are considerably older than present host sediments (<2 Ma) and subducting marine sediments (<21 Ma) in this area, iodine (and, by association, methane in the gas hydrates) must have been derived from source formations located in the continental side of the subduction zone. The results do not support derivation of gas hydrates from present host sediments or currently subducting sediments, but could be related to release and long-time recycling of fluids from marine formations of early Tertiary age.</description><subject>Asia</subject><subject>Cenozoic</subject><subject>Far East</subject><subject>gas hydrates</subject><subject>Gases</subject><subject>geochronology</subject><subject>Geology</subject><subject>halogens</subject><subject>I-129</subject><subject>iodine</subject><subject>isotopes</subject><subject>Japan</subject><subject>Leg 131</subject><subject>Leg 132</subject><subject>Leg 196</subject><subject>marine sediments</subject><subject>mass spectra</subject><subject>Nankai Trough</subject><subject>North Pacific</subject><subject>Northwest Pacific</subject><subject>Ocean Drilling Program</subject><subject>Oceanography</subject><subject>ODP Site 808</subject><subject>Pacific Ocean</subject><subject>pore water</subject><subject>radioactive isotopes</subject><subject>relative age</subject><subject>residence time</subject><subject>sediments</subject><subject>spectra</subject><subject>subduction zones</subject><subject>Tertiary</subject><subject>Water</subject><subject>West Pacific</subject><issn>0091-7613</issn><issn>1943-2682</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNpdkGFr2zAQhkVpYWm6_yD6YWx0Tk-SJdtrGZS0zTLKMmihH4UinRNliZVJDqH_fjYpo_TTHcf7vnf3EHLJYMSYgEuAimWFYuIzBxBfQLBrkJx9m97Ofj_ffOcjGI1nV_yIDFiVi4yrkh-TwX_XB3Ka0gqA5bIoB-RxGpxvkDrT-mZBQ023ISLdmxZjoialYH3XO7r37ZIuTKLLFxe7SaK-oe0S6S_T_DGemojmK_1ptqY5Iye1WSf8-FqH5On-7mn8I3uYTabjm4fMiKJsswrBCaegZlzhPK8UU5WzpS0sKiUBkFmnuLJWiLkq5lIoLMCa2hmY8xzEkHw6xG5j-LvD1OqNTxbXa9Ng2CXdva-klKoTnr8TrsIuNt1pmgNjZal4nzY5iGwMKUWs9Tb6jYkvmoHuweseoe4R6h687sDrHrw-gNdcgx7PNO-SLg5JCwzJemws7kNcu7dbe38upRDiH6mwh3A</recordid><startdate>20030601</startdate><enddate>20030601</enddate><creator>Fehn, Udo</creator><creator>Snyder, Glen T</creator><creator>Matsumoto, Ryo</creator><creator>Muramatsu, Yasuyuki</creator><creator>Tomaru, Hitoshi</creator><general>Geological Society of America (GSA)</general><general>Geological Society of America</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7TN</scope></search><sort><creationdate>20030601</creationdate><title>Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan</title><author>Fehn, Udo ; Snyder, Glen T ; Matsumoto, Ryo ; Muramatsu, Yasuyuki ; Tomaru, Hitoshi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a378t-9e0d3d60f126eb496169dc8c7ce66500e1cd626cc33b67b536e70cafda0b2403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Asia</topic><topic>Cenozoic</topic><topic>Far East</topic><topic>gas hydrates</topic><topic>Gases</topic><topic>geochronology</topic><topic>Geology</topic><topic>halogens</topic><topic>I-129</topic><topic>iodine</topic><topic>isotopes</topic><topic>Japan</topic><topic>Leg 131</topic><topic>Leg 132</topic><topic>Leg 196</topic><topic>marine sediments</topic><topic>mass spectra</topic><topic>Nankai Trough</topic><topic>North Pacific</topic><topic>Northwest Pacific</topic><topic>Ocean Drilling Program</topic><topic>Oceanography</topic><topic>ODP Site 808</topic><topic>Pacific Ocean</topic><topic>pore water</topic><topic>radioactive isotopes</topic><topic>relative age</topic><topic>residence time</topic><topic>sediments</topic><topic>spectra</topic><topic>subduction zones</topic><topic>Tertiary</topic><topic>Water</topic><topic>West Pacific</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Fehn, Udo</creatorcontrib><creatorcontrib>Snyder, Glen T</creatorcontrib><creatorcontrib>Matsumoto, Ryo</creatorcontrib><creatorcontrib>Muramatsu, Yasuyuki</creatorcontrib><creatorcontrib>Tomaru, Hitoshi</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Oceanic Abstracts</collection><jtitle>Geology (Boulder)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fehn, Udo</au><au>Snyder, Glen T</au><au>Matsumoto, Ryo</au><au>Muramatsu, Yasuyuki</au><au>Tomaru, Hitoshi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan</atitle><jtitle>Geology (Boulder)</jtitle><date>2003-06-01</date><risdate>2003</risdate><volume>31</volume><issue>6</issue><spage>521</spage><epage>524</epage><pages>521-524</pages><issn>0091-7613</issn><eissn>1943-2682</eissn><abstract>The Nankai hydrate field, Japan, is an example of gas-hydrate deposits associated with an active subduction zone. In order to determine the origin of gas hydrates in this area, 129I/I ratios together with halogen concentrations were measured in a set of pore-water samples collected from two boreholes in the Nankai hydrate field. Iodine concentrations are between 100 and 230 µM, i.e., strongly enriched compared to seawater, while Cl concentrations were found to be close to that of seawater. Except for one sample, 129I/I ratios are between 180 and 520 × 10-15, giving minimum ages between 24 and 48 Ma. Because these ages are considerably older than present host sediments (<2 Ma) and subducting marine sediments (<21 Ma) in this area, iodine (and, by association, methane in the gas hydrates) must have been derived from source formations located in the continental side of the subduction zone. The results do not support derivation of gas hydrates from present host sediments or currently subducting sediments, but could be related to release and long-time recycling of fluids from marine formations of early Tertiary age.</abstract><cop>Boulder</cop><pub>Geological Society of America (GSA)</pub><doi>10.1130/0091-7613(2003)031<0521:IDOPWA>2.0.CO;2</doi><tpages>4</tpages></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0091-7613 |
ispartof | Geology (Boulder), 2003-06, Vol.31 (6), p.521-524 |
issn | 0091-7613 1943-2682 |
language | eng |
recordid | cdi_proquest_miscellaneous_19465556 |
source | AUTh Library subscriptions: Society of Exploration Geophysicists |
subjects | Asia Cenozoic Far East gas hydrates Gases geochronology Geology halogens I-129 iodine isotopes Japan Leg 131 Leg 132 Leg 196 marine sediments mass spectra Nankai Trough North Pacific Northwest Pacific Ocean Drilling Program Oceanography ODP Site 808 Pacific Ocean pore water radioactive isotopes relative age residence time sediments spectra subduction zones Tertiary Water West Pacific |
title | Iodine dating of pore waters associated with gas hydrates in the Nankai area, Japan |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-11T22%3A19%3A23IST&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=Iodine%20dating%20of%20pore%20waters%20associated%20with%20gas%20hydrates%20in%20the%20Nankai%20area,%20Japan&rft.jtitle=Geology%20(Boulder)&rft.au=Fehn,%20Udo&rft.date=2003-06-01&rft.volume=31&rft.issue=6&rft.spage=521&rft.epage=524&rft.pages=521-524&rft.issn=0091-7613&rft.eissn=1943-2682&rft_id=info:doi/10.1130/0091-7613(2003)031%3C0521:IDOPWA%3E2.0.CO;2&rft_dat=%3Cproquest_cross%3E347538811%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a378t-9e0d3d60f126eb496169dc8c7ce66500e1cd626cc33b67b536e70cafda0b2403%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=201188620&rft_id=info:pmid/&rfr_iscdi=true |