1887

Abstract

Sedimentary reservoir rocks often present heterogeneous pore structures that are inherently related to the original rock<br>texture and subsequent diagenetic alterations. Such alterations are governed by the original rock texture, the involved fluids,<br>the flow history, and the physico-chemical conditions. Throughout the paragenesis, alternating dissolution and precipitation<br>caused by changes in chemical and thermodynamic conditions may lead to heterogeneous rock properties at both local and<br>reservoir scale.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.151.iptc14049
2009-12-07
2024-03-28
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.151.iptc14049
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