Reservoir properties and facies characterization from core data and well logging: autochthonous Miocene sediments in the Carpathian Foredeep case study

Abstract

Laboratory results of total porosity and physical permeability were the basis to calculate Flow Zone Indicator. GR log and porosity log PHI were used for facies identification. Calculations and loggings were performed in the Miocene sandy-shaly sediments in two wells in the Eastern Part of Polish Carpathian Foredeep. FZI increase with the total porosity from the comprehensive interpretation of logs in the regressive set of parasequences was observed. This increase was the result of better reservoir and hydraulic abilities of these parasequences in comparison to transgressive ones. Combining information of laboratory origin with well logging results on the basis of facies and FZI correlation worked also as a kind of data scaling.

Nonlinear anisotropic diffusion techniques for seismic signal enhancing - Carpathian Foredeep study

“…The quality of recorded seismic data was relatively good with a high signal to noise ratio; however, some horizons had been poorly preserved in processed sections. The decreasing quality of the seismic signal in the Jurassic, Cretaceous, and autochthonous Miocene sediments, which are considered as reservoirs in The Carpathian Foredeep, have been noticed [27,28]. As shown in Fig.…”