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<publisher>HAL CCSD</publisher>
<title lang=en>magnetic properties of basalts from Shatsky Rise</title>
<creator>Carvallo, Claire</creator>
<creator>Camps, Pierre</creator>
<contributor>Institut de minéralogie et de physique des milieux condensés (IMPMC) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Manteau et Interfaces ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 1930-1014</source>
<source>Proceedings of the Integrated Ocean Drilling Program</source>
<publisher>Integrated Ocean Drilling Program</publisher>
<identifier>hal-00795484</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00795484</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00795484</source>
<source>Proceedings of the Integrated Ocean Drilling Program, Integrated Ocean Drilling Program, 2013, 324, pp.1. 〈10.2204/iodp.proc.324.201.2013〉</source>
<identifier>DOI : 10.2204/iodp.proc.324.201.2013</identifier>
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<language>en</language>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>A detailed study of magnetic properties was carried out on ~60 samples from three holes cored during Integrated Ocean Drilling Program Expedition 324, Shatsky Rise. The measurements include scanning electron microscopy (SEM), hysteresis, and first-order reversal curve (FORC) diagrams, as well as measurements of susceptibility at high and low temperatures and variation of saturation isothermal magnetization at low temperature. SEM measurements show the presence of a complex mixture of Fe-Ti oxides with various Ti content x, which is confirmed by the measurements of susceptibility variation with temperature and low-temperature measurements. According to FORC diagrams, the magnetization is carried by single-domain to pseudosingle-domain grains.</description>
<date>2013</date>
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