Crustal deformation at the Sumatran Subduction Zone revealed by coral rings
Identifieur interne : 000588 ( Main/Exploration ); précédent : 000587; suivant : 000589Crustal deformation at the Sumatran Subduction Zone revealed by coral rings
Auteurs : Kerry Sieh [États-Unis] ; Steven N. Ward [États-Unis] ; Danny Natawidjaja [Indonésie] ; Bambang W. Suwargadi [Indonésie]Source :
- Geophysical Research Letters [ 0094-8276 ] ; 1999-10-15.
Abstract
Analyses of coral rings grown in the interval 1970–1997 reveal a geographically distinct pattern of interseismic uplift off Sumatra's western coast. At distances less than 110 km from the Sumatran trench, coral reefs are submerging as fast as 5 mm/y. At 130 and 180 km distance from the trench, they are emerging at similar rates. We suggest that a locked, or partially locked patch, located above 30 km depth on the upper surface of the subducting oceanic plate, generates this pattern.
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DOI: 10.1029/1999GL005409
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Lett.</title><idno type="ISSN">0094-8276</idno><idno type="eISSN">1944-8007</idno><imprint><publisher>Blackwell Publishing Ltd</publisher><date type="published" when="1999-10-15">1999-10-15</date><biblScope unit="volume">26</biblScope><biblScope unit="issue">20</biblScope><biblScope unit="page" from="3141">3141</biblScope><biblScope unit="page" to="3144">3144</biblScope></imprint><idno type="ISSN">0094-8276</idno></series><idno type="istex">2EB44D64C2A469C236AC16F090B0E1A9DB87EB42</idno><idno type="DOI">10.1029/1999GL005409</idno><idno type="ArticleID">1999GL005409</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0094-8276</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract">Analyses of coral rings grown in the interval 1970–1997 reveal a geographically distinct pattern of interseismic uplift off Sumatra's western coast. At distances less than 110 km from the Sumatran trench, coral reefs are submerging as fast as 5 mm/y. At 130 and 180 km distance from the trench, they are emerging at similar rates. We suggest that a locked, or partially locked patch, located above 30 km depth on the upper surface of the subducting oceanic plate, generates this pattern.</div></front></TEI><affiliations><list><country><li>Indonésie</li><li>États-Unis</li></country><region><li>Californie</li></region></list><tree><country name="États-Unis"><region name="Californie"><name sortKey="Sieh, Kerry" sort="Sieh, Kerry" uniqKey="Sieh K" first="Kerry" last="Sieh">Kerry Sieh</name></region><name sortKey="Ward, Steven N" sort="Ward, Steven N" uniqKey="Ward S" first="Steven N." last="Ward">Steven N. Ward</name></country><country name="Indonésie"><noRegion><name sortKey="Natawidjaja, Danny" sort="Natawidjaja, Danny" uniqKey="Natawidjaja D" first="Danny" last="Natawidjaja">Danny Natawidjaja</name></noRegion><name sortKey="Suwargadi, Bambang W" sort="Suwargadi, Bambang W" uniqKey="Suwargadi B" first="Bambang W." last="Suwargadi">Bambang W. Suwargadi</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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