1887

Abstract

The historical works in gradient space had 2-D space plots of almost all possible geological structures. Evaluation of recent work by this method for interpretation of a sedimentary basin showed that error entrance caused by lots of approximations must be eliminated. As a more complete and less approximated geometrical interpretation method, 3-D space plots were offered. These kinds of plots contain more details and also they are suitable to use for not only basin but also all dominant anomaly's shape. There isn't any estimation of density in this method because density estimation doesn't appear in this method procedure at all.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.241.mousavi_paper1
2009-09-16
2021-10-17
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.241.mousavi_paper1
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