Bayesian facies inversion on a partially dolomitized isolated carbonate platform: A case study from Central Luconia Province, Malaysia

Author:

Ghon George1ORCID,Grana Dario2ORCID,Rankey Eugene C.3,Baechle Gregor T.4,Bleibinhaus Florian5ORCID,Lang Xiaozheng2,de Figueiredo Leandro Passos6,Poppelreiter Michael C.7

Affiliation:

1. Formerly Montanuniversitaet Leoben, Chair of Applied Geophysics, Leoben 8700, Austria; presently Earth Science Analytics, Stavanger 4021, Norway.(corresponding author).

2. University of Wyoming, Department of Geology and Geophysics, Laramie, Wyoming 82071, USA..

3. University of Kansas, Kansas Interdisciplinary Carbonates Consortium, Lawrence, Kansas 66045, USA..

4. Formerly Repsol, E&P, The Woodlands, Texas 77381, USA; presently Benerco LLC, Houston, Texas 77494, USA..

5. Montanuniversitaet Leoben, Chair of Applied Geophysics, Leoben 8700, Austria..

6. Federal University of Santa Catarina, Physics Department, Florianópolis 88040-900, Brazil and LTrace Geophysical Solutions, Florianópolis 88032-005, Brazil..

7. Shell Kuwait E & P and SEACaRL, Universiti Teknologi Petronas, Seri Iskander 32610, Malaysia..

Abstract

We have developed a case study of geophysical reservoir characterization in which we use elastic inversion and probabilistic prediction to estimate nine carbonate lithofacies and the associated porosity distribution. The study focuses on an isolated carbonate platform of middle Miocene age, offshore Sarawak in Malaysia that has been partly dolomitized — a process that increased the porosity and permeability of the prolific gas reservoir. The nine lithofacies are defined from one reference core and include a range of lithologies and pore types, covering limestone and dolomitized limestone, each with vuggy varieties, as well as sucrosic and crystalline dolomites with intercrystalline porosity, and argillaceous limestones and shales. To predict the lithofacies and porosity from geophysical data, we adopt a probabilistic algorithm that uses Bayesian theory with an analytical solution for conditional means and covariances of posterior probabilities, assuming a Gaussian mixture model. The inversion is a two-step process, first solving for P- and S-wave velocities and density from two partial seismic stacks. Subsequently, the lithofacies and porosity are predicted from the elastic parameters in the borehole and across a 2D inline. The final result is a model that consists of the pointwise posterior distributions of the facies and porosity at each location where seismic data are available. The facies posterior distribution represents the facies proportions estimated from seismic data, whereas the porosity distribution represents the probability density function at each location. These distributions provide the most likely model and its associated uncertainty for geologic interpretations of lithofacies associated with distinct stages of carbonate platform growth.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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