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<front>
<journal-meta>
<journal-id journal-id-type="publisher">SE</journal-id>
<journal-title-group>
<journal-title>Solid Earth</journal-title>
<abbrev-journal-title abbrev-type="publisher">SE</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Solid Earth</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1869-9529</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/se-5-339-2014</article-id>
<title-group>
<article-title>Magnetic signature of large exhumed mantle domains of the Southwest  Indian Ridge &amp;ndash; results from a deep-tow geophysical survey over 0 to 11 Ma old  seafloor</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Bronner</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sauter</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Munschy</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Carlut</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Searle</surname>
<given-names>R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Cannat</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Manatschal</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Université de Strasbourg, Institut de Physique du Globe de  Strasbourg (IPGS) UMR CNRS, Strasbourg, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Sorbonne Paris Cité Université Paris Diderot, Institut de  Physique du Globe de Paris (IPGP), UMR CNRS, Paris, France</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Durham University, Department of Earth Sciences, Durham, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>05</month>
<year>2014</year>
</pub-date>
<volume>5</volume>
<issue>1</issue>
<fpage>339</fpage>
<lpage>354</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 A. Bronner et al.</copyright-statement>
<copyright-year>2014</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://se.copernicus.org/articles/5/339/2014/se-5-339-2014.html">This article is available from https://se.copernicus.org/articles/5/339/2014/se-5-339-2014.html</self-uri>
<self-uri xlink:href="https://se.copernicus.org/articles/5/339/2014/se-5-339-2014.pdf">The full text article is available as a PDF file from https://se.copernicus.org/articles/5/339/2014/se-5-339-2014.pdf</self-uri>
<abstract>
<p>We investigate the magnetic signature of ultramafic seafloor in the
eastern part of the Southwest Indian Ridge (SWIR). There, detachment
faulting, continuous over 11 Myr, exhumed large areas of mantle-derived
rocks. These exhumed mantle domains occur in the form of a smooth rounded
topography with broad ridges locally covered by a thin highly discontinuous
volcanic carapace. We present high-resolution data combining deep-tow
magnetics, side-scan sonar images and dredged samples collected within two
exhumed mantle domains between 62° E and 65° E. We show
that, despite an ultra-slow spreading rate, volcanic areas within robust
magmatic segments are characterized by well-defined seafloor spreading
anomalies. By contrast, the exhumed mantle domains, including a few thin
volcanic patches, reveal a weak and highly variable magnetic pattern. The
analysis of the magnetic properties of the dredged samples and careful
comparison between the nature of the seafloor, the deep-tow magnetic
anomalies and the seafloor equivalent magnetization suggest that the
serpentinized peridotites do not carry a sufficiently stable remanent
magnetization to produce seafloor spreading magnetic anomalies in exhumed
mantle domains.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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