1887
PDF

Abstract

In sand-shale sequences, more sedimentological details could be measured and quantified with an image log, however, vertical resolution has historically been a major limitation in obtaining the data yielded from core analysis or cuttings. As defaults, sedimentological features like cross bedding, lateral accretion and erosion surfaces, and other elements could be identified to define depositional environments for various intervals along the image log. Porosity variations and permeability require additional data be acquired, such as nuclear magnetic resonance or triple-combo logs, but vertical resolution in these logs is limited.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.287.1171903
2012-03-04
2024-04-25
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.287.1171903
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