Building of the Amsterdam‐Saint Paul plateau: A 10 Myr history of a ridge‐hot spot interaction and variations in the strength of the hot spot source
Identifieur interne : 001739 ( Main/Exploration ); précédent : 001738; suivant : 001740Building of the Amsterdam‐Saint Paul plateau: A 10 Myr history of a ridge‐hot spot interaction and variations in the strength of the hot spot source
Auteurs : Marcia Maia [France] ; Ivo Pessanha [France, Brésil] ; Esther Courrèges [France] ; Martin Patriat [France] ; Pascal Gente [France] ; Christophe Hémond [France] ; Myriam Janin [France] ; Kevin Johnson [États-Unis] ; Walter Roest [France] ; Jean-Yves Royer [France] ; Judith Vatteville [France]Source :
- Journal of Geophysical Research: Solid Earth [ 0148-0227 ] ; 2011-09.
Abstract
The Amsterdam‐Saint Paul plateau results from a 10 Myr interaction between the South East Indian Ridge and the Amsterdam‐Saint Paul hot spot. During this period of time, the structure of the plateau changed as a consequence of changes in both the ridge‐hot spot relative distance and in the strength of the hot spot source. The joint analysis of gravity‐derived crust thickness and bathymetry reveals that the plateau started to form at ∼10 Ma by an increase of the crustal production at the ridge axis, due to the nearby hot spot. This phase, which lasted 3–4 Myr, corresponds to a period of a strong hot spot source, maybe due to a high temperature or material flux, and decreasing ridge‐hot spot distance. A second phase, between ∼6 and ∼3 Ma, corresponds to a decrease in the ridge crustal production. During this period, the hot spot center was close to the ridge axis and this reduced magmatic activity suggests a weak hot spot source. At ∼3 Ma, the ridge was located approximately above the hot spot center. An increase in the hot spot source strength then resulted in the building of the shallower part of the plateau. The variations of the melt production at the ridge axis through time resulted in variations in crustal thickness but also in changes in the ridge morphology. The two periods of increased melt production correspond to smooth ridge morphology, characterized by axial highs, while the intermediate period corresponds to a rougher, rift‐valley morphology. These variations reveal changes in axial thermal structure due to higher melting production rates and temperatures.
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DOI: 10.1029/2010JB007768
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Earth</title><title level="j" type="abbrev">J. Geophys. Res.</title><idno type="ISSN">0148-0227</idno><idno type="eISSN">2156-2202</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="2011-09">2011-09</date><biblScope unit="volume">116</biblScope><biblScope unit="issue">B9</biblScope><biblScope unit="page" from="/">n/a</biblScope><biblScope unit="page" to="/">n/a</biblScope></imprint><idno type="ISSN">0148-0227</idno></series><idno type="istex">AF3149E64DDAF61902146ACE80453BF4C74F427E</idno><idno type="DOI">10.1029/2010JB007768</idno><idno type="ArticleID">2010JB007768</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0148-0227</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">The Amsterdam‐Saint Paul plateau results from a 10 Myr interaction between the South East Indian Ridge and the Amsterdam‐Saint Paul hot spot. During this period of time, the structure of the plateau changed as a consequence of changes in both the ridge‐hot spot relative distance and in the strength of the hot spot source. The joint analysis of gravity‐derived crust thickness and bathymetry reveals that the plateau started to form at ∼10 Ma by an increase of the crustal production at the ridge axis, due to the nearby hot spot. This phase, which lasted 3–4 Myr, corresponds to a period of a strong hot spot source, maybe due to a high temperature or material flux, and decreasing ridge‐hot spot distance. A second phase, between ∼6 and ∼3 Ma, corresponds to a decrease in the ridge crustal production. During this period, the hot spot center was close to the ridge axis and this reduced magmatic activity suggests a weak hot spot source. At ∼3 Ma, the ridge was located approximately above the hot spot center. An increase in the hot spot source strength then resulted in the building of the shallower part of the plateau. The variations of the melt production at the ridge axis through time resulted in variations in crustal thickness but also in changes in the ridge morphology. The two periods of increased melt production correspond to smooth ridge morphology, characterized by axial highs, while the intermediate period corresponds to a rougher, rift‐valley morphology. These variations reveal changes in axial thermal structure due to higher melting production rates and temperatures.</div></front></TEI><affiliations><list><country><li>Brésil</li><li>France</li><li>États-Unis</li></country><region><li>Région Bretagne</li><li>Île-de-France</li></region><settlement><li>Paris</li><li>Rennes</li></settlement></list><tree><country name="France"><region name="Région Bretagne"><name sortKey="Maia, Marcia" sort="Maia, Marcia" uniqKey="Maia M" first="Marcia" last="Maia">Marcia Maia</name></region><name sortKey="Courreges, Esther" sort="Courreges, Esther" uniqKey="Courreges E" first="Esther" last="Courrèges">Esther Courrèges</name><name sortKey="Courreges, Esther" sort="Courreges, Esther" uniqKey="Courreges E" first="Esther" last="Courrèges">Esther Courrèges</name><name sortKey="Gente, Pascal" sort="Gente, Pascal" uniqKey="Gente P" first="Pascal" last="Gente">Pascal Gente</name><name sortKey="Gente, Pascal" sort="Gente, Pascal" uniqKey="Gente P" first="Pascal" last="Gente">Pascal Gente</name><name sortKey="Hemond, Christophe" sort="Hemond, Christophe" uniqKey="Hemond C" first="Christophe" last="Hémond">Christophe Hémond</name><name sortKey="Hemond, Christophe" sort="Hemond, Christophe" uniqKey="Hemond C" first="Christophe" last="Hémond">Christophe Hémond</name><name sortKey="Janin, Myriam" sort="Janin, Myriam" uniqKey="Janin M" first="Myriam" last="Janin">Myriam Janin</name><name sortKey="Janin, Myriam" sort="Janin, Myriam" uniqKey="Janin M" first="Myriam" last="Janin">Myriam Janin</name><name sortKey="Janin, Myriam" sort="Janin, Myriam" uniqKey="Janin M" first="Myriam" last="Janin">Myriam Janin</name><name sortKey="Maia, Marcia" sort="Maia, Marcia" uniqKey="Maia M" first="Marcia" last="Maia">Marcia Maia</name><name sortKey="Maia, Marcia" sort="Maia, Marcia" uniqKey="Maia M" first="Marcia" last="Maia">Marcia Maia</name><name sortKey="Patriat, Martin" sort="Patriat, Martin" uniqKey="Patriat M" first="Martin" last="Patriat">Martin Patriat</name><name sortKey="Pessanha, Ivo" sort="Pessanha, Ivo" uniqKey="Pessanha I" first="Ivo" last="Pessanha">Ivo Pessanha</name><name sortKey="Pessanha, Ivo" sort="Pessanha, Ivo" uniqKey="Pessanha I" first="Ivo" last="Pessanha">Ivo Pessanha</name><name sortKey="Roest, Walter" sort="Roest, Walter" uniqKey="Roest W" first="Walter" last="Roest">Walter Roest</name><name sortKey="Royer, Jean Ves" sort="Royer, Jean Ves" uniqKey="Royer J" first="Jean-Yves" last="Royer">Jean-Yves Royer</name><name sortKey="Royer, Jean Ves" sort="Royer, Jean Ves" uniqKey="Royer J" first="Jean-Yves" last="Royer">Jean-Yves Royer</name><name sortKey="Vatteville, Judith" sort="Vatteville, Judith" uniqKey="Vatteville J" first="Judith" last="Vatteville">Judith Vatteville</name></country><country name="Brésil"><noRegion><name sortKey="Pessanha, Ivo" sort="Pessanha, Ivo" uniqKey="Pessanha I" first="Ivo" last="Pessanha">Ivo Pessanha</name></noRegion></country><country name="États-Unis"><noRegion><name sortKey="Johnson, Kevin" sort="Johnson, Kevin" uniqKey="Johnson K" first="Kevin" last="Johnson">Kevin Johnson</name></noRegion></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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