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Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin
Using temperature gradients measured in 10 holes at 6 sites, we generate the first high fidelity heat flow measurements from Integrated Ocean Drilling Program drill holes across the northern and central Lesser Antilles arc and back arc Grenada basin. The implied heat flow, after correcting for bathy...
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Published in: | Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2012-08, Vol.13 (8), p.np-n/a |
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creator | Manga, Michael Hornbach, Matthew J. Le Friant, Anne Ishizuka, Osamu Stroncik, Nicole Adachi, Tatsuya Aljahdali, Mohammed Boudon, Georges Breitkreuz, Christoph Fraass, Andrew Fujinawa, Akihiko Hatfield, Robert Jutzeler, Martin Kataoka, Kyoko Lafuerza, Sara Maeno, Fukashi Martinez-Colon, Michael McCanta, Molly Morgan, Sally Palmer, Martin R. Saito, Takeshi Slagle, Angela Stinton, Adam J. Subramanyam, K. S. V. Tamura, Yoshihiko Talling, Peter J. Villemant, Benoit Wall-Palmer, Deborah Wang, Fei |
description | Using temperature gradients measured in 10 holes at 6 sites, we generate the first high fidelity heat flow measurements from Integrated Ocean Drilling Program drill holes across the northern and central Lesser Antilles arc and back arc Grenada basin. The implied heat flow, after correcting for bathymetry and sedimentation effects, ranges from about 0.1 W/m2 on the crest of the arc, midway between the volcanic islands of Montserrat and Guadeloupe, to 15 km from the crest in the back arc direction. Combined with previous measurements, we find that the magnitude and spatial pattern of heat flow are similar to those at continental arcs. The heat flow in the Grenada basin to the west of the active arc is 0.06 W/m2, a factor of 2 lower than that found in the previous and most recent study. There is no thermal evidence for significant shallow fluid advection at any of these sites. Present‐day volcanism is confined to the region with the highest heat flow.
Key Points
Heat flow in the Lesser Antilles is similar to other volcanic arcs
No evidence for subsurface fluid flow
Volcanism is confined to the region with high heat flow |
doi_str_mv | 10.1029/2012GC004260 |
format | article |
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Key Points
Heat flow in the Lesser Antilles is similar to other volcanic arcs
No evidence for subsurface fluid flow
Volcanism is confined to the region with high heat flow</description><identifier>ISSN: 1525-2027</identifier><identifier>EISSN: 1525-2027</identifier><identifier>DOI: 10.1029/2012GC004260</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Arc heating ; back arc ; Basins ; Earth Sciences ; Fluid dynamics ; Fluid flow ; Grenada basin ; heat flow ; Heat transfer ; Heat transmission ; IODP ; Islands ; Lesser Antilles ; Sciences of the Universe ; volcanic arc</subject><ispartof>Geochemistry, geophysics, geosystems : G3, 2012-08, Vol.13 (8), p.np-n/a</ispartof><rights>2012. American Geophysical Union. All Rights Reserved.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a5714-98e85bee2dd1d2221bb1b33c250e8d466317dd91c5e39d7eb3b4374bf3c10bfc3</citedby><cites>FETCH-LOGICAL-a5714-98e85bee2dd1d2221bb1b33c250e8d466317dd91c5e39d7eb3b4374bf3c10bfc3</cites><orcidid>0000-0001-6150-5625 ; 0000-0003-2126-6505 ; 0000-0001-6550-7222 ; 0000-0003-3286-4682 ; 0000-0001-8901-2515</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2012GC004260$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2012GC004260$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,315,786,790,891,27957,27958,50923,51032</link.rule.ids><backlink>$$Uhttps://hal.science/hal-00796877$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Manga, Michael</creatorcontrib><creatorcontrib>Hornbach, Matthew J.</creatorcontrib><creatorcontrib>Le Friant, Anne</creatorcontrib><creatorcontrib>Ishizuka, Osamu</creatorcontrib><creatorcontrib>Stroncik, Nicole</creatorcontrib><creatorcontrib>Adachi, Tatsuya</creatorcontrib><creatorcontrib>Aljahdali, Mohammed</creatorcontrib><creatorcontrib>Boudon, Georges</creatorcontrib><creatorcontrib>Breitkreuz, Christoph</creatorcontrib><creatorcontrib>Fraass, Andrew</creatorcontrib><creatorcontrib>Fujinawa, Akihiko</creatorcontrib><creatorcontrib>Hatfield, Robert</creatorcontrib><creatorcontrib>Jutzeler, Martin</creatorcontrib><creatorcontrib>Kataoka, Kyoko</creatorcontrib><creatorcontrib>Lafuerza, Sara</creatorcontrib><creatorcontrib>Maeno, Fukashi</creatorcontrib><creatorcontrib>Martinez-Colon, Michael</creatorcontrib><creatorcontrib>McCanta, Molly</creatorcontrib><creatorcontrib>Morgan, Sally</creatorcontrib><creatorcontrib>Palmer, Martin R.</creatorcontrib><creatorcontrib>Saito, Takeshi</creatorcontrib><creatorcontrib>Slagle, Angela</creatorcontrib><creatorcontrib>Stinton, Adam J.</creatorcontrib><creatorcontrib>Subramanyam, K. S. V.</creatorcontrib><creatorcontrib>Tamura, Yoshihiko</creatorcontrib><creatorcontrib>Talling, Peter J.</creatorcontrib><creatorcontrib>Villemant, Benoit</creatorcontrib><creatorcontrib>Wall-Palmer, Deborah</creatorcontrib><creatorcontrib>Wang, Fei</creatorcontrib><title>Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin</title><title>Geochemistry, geophysics, geosystems : G3</title><addtitle>Geochem. Geophys. Geosyst</addtitle><description>Using temperature gradients measured in 10 holes at 6 sites, we generate the first high fidelity heat flow measurements from Integrated Ocean Drilling Program drill holes across the northern and central Lesser Antilles arc and back arc Grenada basin. The implied heat flow, after correcting for bathymetry and sedimentation effects, ranges from about 0.1 W/m2 on the crest of the arc, midway between the volcanic islands of Montserrat and Guadeloupe, to <0.07 W/m2 at distances >15 km from the crest in the back arc direction. Combined with previous measurements, we find that the magnitude and spatial pattern of heat flow are similar to those at continental arcs. The heat flow in the Grenada basin to the west of the active arc is 0.06 W/m2, a factor of 2 lower than that found in the previous and most recent study. There is no thermal evidence for significant shallow fluid advection at any of these sites. Present‐day volcanism is confined to the region with the highest heat flow.
Key Points
Heat flow in the Lesser Antilles is similar to other volcanic arcs
No evidence for subsurface fluid flow
Volcanism is confined to the region with high heat flow</description><subject>Arc heating</subject><subject>back arc</subject><subject>Basins</subject><subject>Earth Sciences</subject><subject>Fluid dynamics</subject><subject>Fluid flow</subject><subject>Grenada basin</subject><subject>heat flow</subject><subject>Heat transfer</subject><subject>Heat transmission</subject><subject>IODP</subject><subject>Islands</subject><subject>Lesser Antilles</subject><subject>Sciences of the Universe</subject><subject>volcanic arc</subject><issn>1525-2027</issn><issn>1525-2027</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNqFkU1rFEEQhgdRMEZv_oAGLwqOdvXnzHFZ4qyway6K3pr-qCG9mczE7tnE_Ht7MxKCBz1V8fJU8b5VVfUa6AegrP3IKLBuTalgij6pTkAyWTPK9NNH_fPqRc57SkFI2ZxU5xu0M-mH6ZbEkcwXSLaYMyayGuc4DJhJzIMdA7HJk_sa9tbjOBNn_eW92iUcbbBFyHF8WT3r7ZDx1Z96Wn37dPZ1vam3593n9WpbW6lB1G2DjXSILAQIjDFwDhznnkmKTRBKcdAhtOAl8jZodNwJroXruQfqes9Pq3fL3gs7mOsUr2y6M5ONZrPamqNGqW5Vo_UNFPbtwl6n6ecB82yuYvY4lFw4HbIBJRhrgTXi_6hkQgAoygv65i90Px3SWEIb0KrcF6RqCvV-oXyack7YP5gFao5PM4-fVnC24LdxwLt_sqbrurPi-2i6XoZinvHXw5BNl0ZprqX5_qUzYgM_dmy3M5z_BsRZovA</recordid><startdate>201208</startdate><enddate>201208</enddate><creator>Manga, Michael</creator><creator>Hornbach, Matthew J.</creator><creator>Le Friant, Anne</creator><creator>Ishizuka, Osamu</creator><creator>Stroncik, Nicole</creator><creator>Adachi, Tatsuya</creator><creator>Aljahdali, Mohammed</creator><creator>Boudon, Georges</creator><creator>Breitkreuz, Christoph</creator><creator>Fraass, Andrew</creator><creator>Fujinawa, Akihiko</creator><creator>Hatfield, Robert</creator><creator>Jutzeler, Martin</creator><creator>Kataoka, Kyoko</creator><creator>Lafuerza, Sara</creator><creator>Maeno, Fukashi</creator><creator>Martinez-Colon, Michael</creator><creator>McCanta, Molly</creator><creator>Morgan, Sally</creator><creator>Palmer, Martin R.</creator><creator>Saito, Takeshi</creator><creator>Slagle, Angela</creator><creator>Stinton, Adam J.</creator><creator>Subramanyam, K. S. V.</creator><creator>Tamura, Yoshihiko</creator><creator>Talling, Peter J.</creator><creator>Villemant, Benoit</creator><creator>Wall-Palmer, Deborah</creator><creator>Wang, Fei</creator><general>Blackwell Publishing Ltd</general><general>John Wiley & Sons, Inc</general><general>AGU and the Geochemical Society</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0001-6150-5625</orcidid><orcidid>https://orcid.org/0000-0003-2126-6505</orcidid><orcidid>https://orcid.org/0000-0001-6550-7222</orcidid><orcidid>https://orcid.org/0000-0003-3286-4682</orcidid><orcidid>https://orcid.org/0000-0001-8901-2515</orcidid></search><sort><creationdate>201208</creationdate><title>Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin</title><author>Manga, Michael ; Hornbach, Matthew J. ; Le Friant, Anne ; Ishizuka, Osamu ; Stroncik, Nicole ; Adachi, Tatsuya ; Aljahdali, Mohammed ; Boudon, Georges ; Breitkreuz, Christoph ; Fraass, Andrew ; Fujinawa, Akihiko ; Hatfield, Robert ; Jutzeler, Martin ; Kataoka, Kyoko ; Lafuerza, Sara ; Maeno, Fukashi ; Martinez-Colon, Michael ; McCanta, Molly ; Morgan, Sally ; Palmer, Martin R. ; Saito, Takeshi ; Slagle, Angela ; Stinton, Adam J. ; Subramanyam, K. S. V. ; Tamura, Yoshihiko ; Talling, Peter J. ; Villemant, Benoit ; Wall-Palmer, Deborah ; Wang, Fei</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a5714-98e85bee2dd1d2221bb1b33c250e8d466317dd91c5e39d7eb3b4374bf3c10bfc3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Arc heating</topic><topic>back arc</topic><topic>Basins</topic><topic>Earth Sciences</topic><topic>Fluid dynamics</topic><topic>Fluid flow</topic><topic>Grenada basin</topic><topic>heat flow</topic><topic>Heat transfer</topic><topic>Heat transmission</topic><topic>IODP</topic><topic>Islands</topic><topic>Lesser Antilles</topic><topic>Sciences of the Universe</topic><topic>volcanic arc</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Manga, Michael</creatorcontrib><creatorcontrib>Hornbach, Matthew J.</creatorcontrib><creatorcontrib>Le Friant, Anne</creatorcontrib><creatorcontrib>Ishizuka, Osamu</creatorcontrib><creatorcontrib>Stroncik, Nicole</creatorcontrib><creatorcontrib>Adachi, Tatsuya</creatorcontrib><creatorcontrib>Aljahdali, Mohammed</creatorcontrib><creatorcontrib>Boudon, Georges</creatorcontrib><creatorcontrib>Breitkreuz, Christoph</creatorcontrib><creatorcontrib>Fraass, Andrew</creatorcontrib><creatorcontrib>Fujinawa, Akihiko</creatorcontrib><creatorcontrib>Hatfield, Robert</creatorcontrib><creatorcontrib>Jutzeler, Martin</creatorcontrib><creatorcontrib>Kataoka, Kyoko</creatorcontrib><creatorcontrib>Lafuerza, Sara</creatorcontrib><creatorcontrib>Maeno, Fukashi</creatorcontrib><creatorcontrib>Martinez-Colon, Michael</creatorcontrib><creatorcontrib>McCanta, Molly</creatorcontrib><creatorcontrib>Morgan, Sally</creatorcontrib><creatorcontrib>Palmer, Martin R.</creatorcontrib><creatorcontrib>Saito, Takeshi</creatorcontrib><creatorcontrib>Slagle, Angela</creatorcontrib><creatorcontrib>Stinton, Adam J.</creatorcontrib><creatorcontrib>Subramanyam, K. S. V.</creatorcontrib><creatorcontrib>Tamura, Yoshihiko</creatorcontrib><creatorcontrib>Talling, Peter J.</creatorcontrib><creatorcontrib>Villemant, Benoit</creatorcontrib><creatorcontrib>Wall-Palmer, Deborah</creatorcontrib><creatorcontrib>Wang, Fei</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</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>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Geochemistry, geophysics, geosystems : G3</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Manga, Michael</au><au>Hornbach, Matthew J.</au><au>Le Friant, Anne</au><au>Ishizuka, Osamu</au><au>Stroncik, Nicole</au><au>Adachi, Tatsuya</au><au>Aljahdali, Mohammed</au><au>Boudon, Georges</au><au>Breitkreuz, Christoph</au><au>Fraass, Andrew</au><au>Fujinawa, Akihiko</au><au>Hatfield, Robert</au><au>Jutzeler, Martin</au><au>Kataoka, Kyoko</au><au>Lafuerza, Sara</au><au>Maeno, Fukashi</au><au>Martinez-Colon, Michael</au><au>McCanta, Molly</au><au>Morgan, Sally</au><au>Palmer, Martin R.</au><au>Saito, Takeshi</au><au>Slagle, Angela</au><au>Stinton, Adam J.</au><au>Subramanyam, K. S. V.</au><au>Tamura, Yoshihiko</au><au>Talling, Peter J.</au><au>Villemant, Benoit</au><au>Wall-Palmer, Deborah</au><au>Wang, Fei</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin</atitle><jtitle>Geochemistry, geophysics, geosystems : G3</jtitle><addtitle>Geochem. Geophys. Geosyst</addtitle><date>2012-08</date><risdate>2012</risdate><volume>13</volume><issue>8</issue><spage>np</spage><epage>n/a</epage><pages>np-n/a</pages><issn>1525-2027</issn><eissn>1525-2027</eissn><notes>istex:5D1CFD2E78C9512B7CF042FED6F6D89604463F59</notes><notes>ark:/67375/WNG-4H1XM2MM-3</notes><notes>ArticleID:2012GC004260</notes><notes>Tab-delimited Table 1.Tab-delimited Table 2.Tab-delimited Table 3.Tab-delimited Table 4.</notes><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><abstract>Using temperature gradients measured in 10 holes at 6 sites, we generate the first high fidelity heat flow measurements from Integrated Ocean Drilling Program drill holes across the northern and central Lesser Antilles arc and back arc Grenada basin. The implied heat flow, after correcting for bathymetry and sedimentation effects, ranges from about 0.1 W/m2 on the crest of the arc, midway between the volcanic islands of Montserrat and Guadeloupe, to <0.07 W/m2 at distances >15 km from the crest in the back arc direction. Combined with previous measurements, we find that the magnitude and spatial pattern of heat flow are similar to those at continental arcs. The heat flow in the Grenada basin to the west of the active arc is 0.06 W/m2, a factor of 2 lower than that found in the previous and most recent study. There is no thermal evidence for significant shallow fluid advection at any of these sites. Present‐day volcanism is confined to the region with the highest heat flow.
Key Points
Heat flow in the Lesser Antilles is similar to other volcanic arcs
No evidence for subsurface fluid flow
Volcanism is confined to the region with high heat flow</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2012GC004260</doi><tpages>19</tpages><orcidid>https://orcid.org/0000-0001-6150-5625</orcidid><orcidid>https://orcid.org/0000-0003-2126-6505</orcidid><orcidid>https://orcid.org/0000-0001-6550-7222</orcidid><orcidid>https://orcid.org/0000-0003-3286-4682</orcidid><orcidid>https://orcid.org/0000-0001-8901-2515</orcidid><oa>free_for_read</oa></addata></record> |
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language | eng |
recordid | cdi_hal_primary_oai_HAL_hal_00796877v1 |
source | Wiley; Alma/SFX Local Collection |
subjects | Arc heating back arc Basins Earth Sciences Fluid dynamics Fluid flow Grenada basin heat flow Heat transfer Heat transmission IODP Islands Lesser Antilles Sciences of the Universe volcanic arc |
title | Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin |
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