1887
PDF

Abstract

Continental rifting and the Early Cretaceous opening of the South Atlantic formed<br>the passive, volcanic margin off Namibia. Just prior to the onset of sea floor<br>spreading a Large Igneous Province emplaced including voluminous extrusives,<br>continental flood basalts and subvolcanic ring complexes. Multichannel seismic<br>reflection and wide-angle data were collected to explore the deep structure of the<br>entire continent-ocean transition. This contribution presents preliminary results<br>from P-velocity modelling and inversion.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.223.009
1997-09-29
2024-04-25
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.223.009
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error