- Accueil >
- Maalama Textuelle >
- Développement durable >
- Environnement >
- Lithosphère >
- Croûte terrestre >
- Activités sismiques >
- Lithosphere delamination with foundering of lower crust and mantle caused permanent subsidence of New Caledonia Trough and transient uplift of Lord Howe Rise during Eocene and Oligocene initiation of Tonga-Kermadec subduction, western Pacific
Lithosphere delamination with foundering of lower crust and mantle caused permanent subsidence of New Caledonia Trough and transient uplift of Lord Howe Rise during Eocene and Oligocene initiation of Tonga-Kermadec subduction, western Pacific
Auteur :
Sutherland
Rupert,
Collot
Julien,
Lafoy
Yves,
...[et al.]
Année de Publication :
2010
Type : Article
Thème : Lithosphère
Couverture :
Australie
URL Article :
http://archimer.ifremer.fr/doc/00001/11271/9283.pdfURL Source :
http://archimer.ifremer.fr 
Télécharger le document :
(2,02 MB) lithosphere_delamination_foudering_lower_crust_mantle.pdfRésumé/Sommaire :
Summary
1. Introduction
2. Geology of New Zealand
3. Geology of New Caledonia
4. Offshore Crust Type and Thickness
5. Stratigraphy of Lord Howe Rise
6. Stratigraphy and Structure of New Caledonia Trough
7. Evidence for Large Values of Tectonic Subsidence
8. Requirement for a Two‐Phase Tectonic Model
9. A New Hypothesis: Delamination of the Lithosphere
10. Lithospheric Delamination in a Global Context
11. Conclusion
References.
- Plan du site -
- HCP -
- CND -
- Qui sommes nous-
- FAQ-
- RSS
