The article provides uplift timing data for the worlds major uplifted cratons, and with a geodynamic model shows that this uplift is likely caused by mantle convection caused by continental rifting and breakup
Coevolution of craton margins and interiors during continental break-up / Gernon, T.M., Hincks, T.K., Brune, S., Braun, J., Jones, S.M., Keir, D., Cunningham, A., Glerum, A,. - In: NATURE. - ISSN 1476-4687. - ELETTRONICO. - 632:(2024), pp. 327-335. [10.1038/s41586-024-07717-1]
Coevolution of craton margins and interiors during continental break-up
Keir D.Writing – Review & Editing
;
2024
Abstract
The article provides uplift timing data for the worlds major uplifted cratons, and with a geodynamic model shows that this uplift is likely caused by mantle convection caused by continental rifting and breakup
File in questo prodotto:
| File | Dimensione | Formato | |
|---|---|---|---|
|
s41586-024-07717-1_s.pdf
accesso aperto
Tipologia:
Pdf editoriale (Version of record)
Licenza:
Open Access
Dimensione
5.68 MB
Formato
Adobe PDF
|
5.68 MB | Adobe PDF |
I documenti in FLORE sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
