1887

Abstract

The subsurface facies analysis was based on a single well penetrating the Late Oligocene K1 – K10 sands of the Penyu Formation in the Eastern reaches of the Penyu Basin. This well acquired an extensive data suite including; conventional wireline (gamma-ray, lateralog resistivity, density-neutron, acoustic), specialized data such as electrical imaging, nuclear magnetic resonance, elemental capture spectroscopy and dielectric propogation. In addition, the entire reservoir succession was conventionally cored and drill-stem tested. The borehole conditions were good and therefore the data quality was excellent for detailed facies analysis. The image log was calibrated to core, and detailed facies analysis was extended beyond the core using the geological features from the images, the porosity and permeability from conventional density-neutron and the nuclear magnetic tool and the mineralogy from the elemental capture spectroscopy.Three major lithological groups were identified sandstone, heterolithic and mudstone with each facies often transitional to the next. The overall depositional environment has been interpreted as restricted shallow marginal marine bay adjacent or proximal to a low energy delta or estuarine mouth.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.340.P29
2013-03-18
2024-03-29
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.340.P29
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