untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T15:42:48Z</responseDate>
<request identifier=oai:HAL:insu-00338254v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:insu-00338254v1</identifier>
<datestamp>2018-01-11</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>subject:sde</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:SDE</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:UNIV-ORLEANS</setSpec>
<setSpec>collection:ISTO</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:OSUC</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:UPMC</setSpec>
<setSpec>collection:UNIV-PARIS7</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:IPGP</setSpec>
<setSpec>collection:USPC</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>Miocene to present kinematics of fault-bend folding across the Huerguosi anticline, northern Tianshan (China), derived from structural, seismic, and magnetostratigraphic data</title>
<creator>Charreau, Julien</creator>
<creator>Avouac, Jean-Philippe</creator>
<creator>Chen, Yan</creator>
<creator>Dominguez, Stéphane</creator>
<creator>Gilder, Stuart, </creator>
<contributor>Institut des Sciences de la Terre d'Orléans (ISTO) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Division of Geological and Planetary Sciences [Pasadena] ; California Institute of Technology (CALTECH)</contributor>
<contributor>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)</contributor>
<contributor>Institut de Physique du Globe de Paris (IPGP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>ECLIPSE-INSU</contributor>
<description>International audience</description>
<source>ISSN: 0091-7613</source>
<source>EISSN: 0091-7613</source>
<source>Geology</source>
<publisher>Geological Society of America</publisher>
<identifier>insu-00338254</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00338254</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-00338254</source>
<source>Geology, Geological Society of America, 2008, 36 (11), pp.871-874. 〈10.1130/G25073A.1〉</source>
<identifier>DOI : 10.1130/G25073A.1</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1130/G25073A.1</relation>
<language>en</language>
<subject>91.45.Dh</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>We combine surface structural measurements, subsurface seismic imaging, and magneto-stratigraphic dating to retrieve, through geometric modeling, the detailed history of fold growth and sedimentation across the Huerguosi anticline, on the northern Tianshan piedmont, taking advantage of a beautifully exposed section of growth strata. The model assumes a fault-bend folding mechanism, consistent with subsurface fold geometry. The shortening history is obtained by least-squares fitting of the measured dip angles of the growth strata. The shortening rate across the anticline is shown to have been remarkably constant: it increased only slightly from 0.84 ± 0.04 mm/yr between 10 and 4 Ma to 1.14 ± 0.02 mm/yr over the past 4 m.y. This approach also allows correcting syntectonic sedimentation rates for the effect of the fold growth and shows that the sedimentation rates in the piggyback basin increased abruptly from ~0.4 to ~0.7 mm/yr ca. 4 Ma.</description>
<date>2008</date>
<contributor>ANR-05-BLAN-0143-01, ANR-05-BLAN-0143-01</contributor>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
