Serveur d'exploration Cyberinfrastructure

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model

Identifieur interne : 000387 ( Main/Exploration ); précédent : 000386; suivant : 000388

The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model

Auteurs : Ana D. Gibbons [Australie] ; Joanne M. Whittaker [Australie] ; R. Dietmar Müller [Australie]

Source :

RBID : ISTEX:D4E299E749399FF0C56394DC3B683C0BEF2F0C44

Abstract

Published models for the Cretaceous seafloor‐spreading history of East Gondwana result in unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate particular constraints from at least one of the associated ocean basins. We link East Gondwana spreading corridors by integrating magnetic and gravity anomaly data from the Enderby Basin off East Antarctica within a regional plate kinematic framework to identify a conjugate series of east‐west‐trending magnetic anomalies, M4 to M0 (~126.7–120.4 Ma). The mid‐ocean ridge that separated Greater India from Australia‐Antarctica propagated from north to south, starting at ~136 Ma northwest of Australia, and reached the southern tip of India at ~126 Ma. Seafloor spreading in the Enderby Basin was abandoned at ~115 Ma, when a ridge jump transferred the Elan Bank and South Kerguelen Plateau to the Antarctic plate. Our revised plate kinematic model helps resolve the problem of successive two‐way strike‐slip motion between Madagascar and India seen in many previously published reconstructions and also suggests that seafloor spreading between them progressed from south to north from 94 to 84 Ma. This timing is essential for tectonic flow lines to match the curved fracture zones of the Wharton and Enderby basins, as Greater India gradually began to unzip from Madagascar from ~100 Ma. In our model, the 85‐East Ridge and Kerguelen Fracture Zone formed as conjugate flanks of a “leaky” transform fault following the ~100 Ma spreading reorganization. Our model also identifies the Afanasy Nikitin Seamounts as products of the Conrad Rise hotspot.

Url:
DOI: 10.1002/jgrb.50079


Affiliations:


Links toward previous steps (curation, corpus...)


Le document en format XML

<record>
<TEI wicri:istexFullTextTei="biblStruct">
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en">The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model</title>
<author>
<name sortKey="Gibbons, Ana D" sort="Gibbons, Ana D" uniqKey="Gibbons A" first="Ana D." last="Gibbons">Ana D. Gibbons</name>
</author>
<author>
<name sortKey="Whittaker, Joanne M" sort="Whittaker, Joanne M" uniqKey="Whittaker J" first="Joanne M." last="Whittaker">Joanne M. Whittaker</name>
</author>
<author>
<name sortKey="Muller, R Dietmar" sort="Muller, R Dietmar" uniqKey="Muller R" first="R. Dietmar" last="Müller">R. Dietmar Müller</name>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:D4E299E749399FF0C56394DC3B683C0BEF2F0C44</idno>
<date when="2013" year="2013">2013</date>
<idno type="doi">10.1002/jgrb.50079</idno>
<idno type="url">https://api.istex.fr/document/D4E299E749399FF0C56394DC3B683C0BEF2F0C44/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">000636</idno>
<idno type="wicri:Area/Istex/Curation">000636</idno>
<idno type="wicri:Area/Istex/Checkpoint">000006</idno>
<idno type="wicri:doubleKey">2169-9313:2013:Gibbons A:the:breakup:of</idno>
<idno type="wicri:Area/Main/Merge">000388</idno>
<idno type="wicri:Area/Main/Curation">000387</idno>
<idno type="wicri:Area/Main/Exploration">000387</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title level="a" type="main" xml:lang="en">The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model</title>
<author>
<name sortKey="Gibbons, Ana D" sort="Gibbons, Ana D" uniqKey="Gibbons A" first="Ana D." last="Gibbons">Ana D. Gibbons</name>
<affiliation wicri:level="3">
<country xml:lang="fr">Australie</country>
<wicri:regionArea>EarthByte Group, School of Geosciences, University of Sydney, NSW, 2006, Sydney</wicri:regionArea>
<placeName>
<settlement type="city">Sydney</settlement>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Whittaker, Joanne M" sort="Whittaker, Joanne M" uniqKey="Whittaker J" first="Joanne M." last="Whittaker">Joanne M. Whittaker</name>
<affiliation wicri:level="3">
<country xml:lang="fr">Australie</country>
<wicri:regionArea>EarthByte Group, School of Geosciences, University of Sydney, NSW, 2006, Sydney</wicri:regionArea>
<placeName>
<settlement type="city">Sydney</settlement>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Muller, R Dietmar" sort="Muller, R Dietmar" uniqKey="Muller R" first="R. Dietmar" last="Müller">R. Dietmar Müller</name>
<affiliation wicri:level="3">
<country xml:lang="fr">Australie</country>
<wicri:regionArea>EarthByte Group, School of Geosciences, University of Sydney, NSW, 2006, Sydney</wicri:regionArea>
<placeName>
<settlement type="city">Sydney</settlement>
</placeName>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Journal of Geophysical Research: Solid Earth</title>
<title level="j" type="abbrev">J. Geophys. Res. Solid Earth</title>
<idno type="ISSN">2169-9313</idno>
<idno type="eISSN">2169-9356</idno>
<imprint>
<publisher>Blackwell Publishing Ltd</publisher>
<date type="published" when="2013-03">2013-03</date>
<biblScope unit="volume">118</biblScope>
<biblScope unit="issue">3</biblScope>
<biblScope unit="page" from="808">808</biblScope>
<biblScope unit="page" to="822">822</biblScope>
</imprint>
<idno type="ISSN">2169-9313</idno>
</series>
<idno type="istex">D4E299E749399FF0C56394DC3B683C0BEF2F0C44</idno>
<idno type="DOI">10.1002/jgrb.50079</idno>
<idno type="ArticleID">JGRB50079</idno>
</biblStruct>
</sourceDesc>
<seriesStmt>
<idno type="ISSN">2169-9313</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass></textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract">Published models for the Cretaceous seafloor‐spreading history of East Gondwana result in unlikely tectonic scenarios for at least one of the plate boundaries involved and/or violate particular constraints from at least one of the associated ocean basins. We link East Gondwana spreading corridors by integrating magnetic and gravity anomaly data from the Enderby Basin off East Antarctica within a regional plate kinematic framework to identify a conjugate series of east‐west‐trending magnetic anomalies, M4 to M0 (~126.7–120.4 Ma). The mid‐ocean ridge that separated Greater India from Australia‐Antarctica propagated from north to south, starting at ~136 Ma northwest of Australia, and reached the southern tip of India at ~126 Ma. Seafloor spreading in the Enderby Basin was abandoned at ~115 Ma, when a ridge jump transferred the Elan Bank and South Kerguelen Plateau to the Antarctic plate. Our revised plate kinematic model helps resolve the problem of successive two‐way strike‐slip motion between Madagascar and India seen in many previously published reconstructions and also suggests that seafloor spreading between them progressed from south to north from 94 to 84 Ma. This timing is essential for tectonic flow lines to match the curved fracture zones of the Wharton and Enderby basins, as Greater India gradually began to unzip from Madagascar from ~100 Ma. In our model, the 85‐East Ridge and Kerguelen Fracture Zone formed as conjugate flanks of a “leaky” transform fault following the ~100 Ma spreading reorganization. Our model also identifies the Afanasy Nikitin Seamounts as products of the Conrad Rise hotspot.</div>
</front>
</TEI>
<affiliations>
<list>
<country>
<li>Australie</li>
</country>
<settlement>
<li>Sydney</li>
</settlement>
</list>
<tree>
<country name="Australie">
<noRegion>
<name sortKey="Gibbons, Ana D" sort="Gibbons, Ana D" uniqKey="Gibbons A" first="Ana D." last="Gibbons">Ana D. Gibbons</name>
</noRegion>
<name sortKey="Muller, R Dietmar" sort="Muller, R Dietmar" uniqKey="Muller R" first="R. Dietmar" last="Müller">R. Dietmar Müller</name>
<name sortKey="Whittaker, Joanne M" sort="Whittaker, Joanne M" uniqKey="Whittaker J" first="Joanne M." last="Whittaker">Joanne M. Whittaker</name>
</country>
</tree>
</affiliations>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Ticri/CIDE/explor/CyberinfraV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 000387 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 000387 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Ticri/CIDE
   |area=    CyberinfraV1
   |flux=    Main
   |étape=   Exploration
   |type=    RBID
   |clé=     ISTEX:D4E299E749399FF0C56394DC3B683C0BEF2F0C44
   |texte=   The breakup of East Gondwana: Assimilating constraints from Cretaceous ocean basins around India into a best‐fit tectonic model
}}

Wicri

This area was generated with Dilib version V0.6.25.
Data generation: Thu Oct 27 09:30:58 2016. Site generation: Sun Mar 10 23:08:40 2024