1887

Abstract

The sedimentary record of the offshore part of continental margins is characterized by important thermic subsidence, which favours a good preservation of sedimentary sequences (contrarily to the onshore part of margins). This sedimentation in turns enhances the subsidence because of loading effects. The quantification of this total postrift subsidence (and the relative effect of both factors) is not always easy, especially when no wells are available in the area. We present here a method based on sedimentary Markers, in the Gulf of Lion.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.172.SBGF0443_07
2007-11-19
2024-03-29
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.172.SBGF0443_07
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