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  2. 01 学術雑誌論文
  1. 360 災害・復興科学研究所
  2. 10 学術雑誌論文
  3. 10 査読済論文

Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin

http://hdl.handle.net/10191/30469
http://hdl.handle.net/10191/30469
1b39486c-b0f5-448f-834d-29e5c3d34180
名前 / ファイル ライセンス アクション
13_8_GC004260.pdf 13_8_GC004260.pdf (770.7 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2014-11-19
タイトル
タイトル Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin
タイトル
タイトル Heat flow in the Lesser Antilles island arc and adjacent back arc Grenada basin
言語 en
言語
言語 eng
キーワード
主題Scheme Other
主題 Grenada basin
キーワード
主題Scheme Other
主題 IODP
キーワード
主題Scheme Other
主題 Lesser Antilles
キーワード
主題Scheme Other
主題 back arc
キーワード
主題Scheme Other
主題 heat flow
キーワード
主題Scheme Other
主題 volcanic art
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 Manga, Michael

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Manga, Michael

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Hornbach, Matthew J.

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Friant, Anne Le

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Ishizuka, Osamu

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Ishizuka, Osamu

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Stroncik, Nicole

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Adachi, Tatsuya

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Aljahdali, Mohammed

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Boudon, Georges

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Breitkreuz, Christoph

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Fraass, Andrew

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Fujinawa, Akihiko

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Hatfield, Robert

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Jutzeler, Martin

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Kataoka, Kyoko

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Lafuerza, Sara

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Maeno, Fukashi

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Martinez-Colon, Michael

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McCanta, Molly

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Morgan, Sally

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Palmer, Martin R.

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Saito, Takeshi

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Slagle, Angela

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Stinton, Adam J.

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Subramanyam, K. S. V.

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Tamura, Yoshihiko

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Talling, Peter J.

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Villemant, Benoit

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Wall-Palmer, Deborah

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Wang, Fei

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抄録
内容記述タイプ Abstract
内容記述 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.
書誌情報 Geochemistry, Geophysics, Geosystems
en : Geochemistry, Geophysics, Geosystems

巻 13, 号 8, p. GC004260-1-GC004260-19, 発行日 2012-08
出版者
出版者 American Geophysical Union
ISSN
収録物識別子タイプ ISSN
収録物識別子 15252027
DOI
識別子タイプ DOI
関連識別子 info:doi/10.1029/2012GC004260
権利
権利情報 Copyright(C)2012 American Geophysical Union
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