1887
PDF

Abstract

It is commonly considered that reservoir properties of Peritethyan carbonates mostly originated<br>from intense dissolution (vugs, molds, enlarged fractures, caverns) in a variety meteoric<br>diagenetic environments. This dissolution took place prior to the burial by non-reservoir or seal<br>units, under unconformities of different orders of magnitude or in shallow, near-surface aquifers.<br>Primary depositional porosities are seen as extensively obliterated by cementation and<br>compaction.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201405769
2002-05-27
2022-11-30
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405769
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