1887

Abstract

Summary

Low permeability carbonate reservoirs constitutes significant reserves of oil and gas for Petrobras’ E&P sector. Micro-porosities above ~ 10% in these sedimentary sequences allow the accumulation of significant volumes of hydrocarbon. However, the predominance of pore throats smaller than 10 microns produces low permeability in this type of rock, making it difficult for the flow of interstitial fluid during production. This constitutes the main challenge for making production feasible. The shortage of static and dynamic data in most reservoirs of low permeability makes it extremely difficult to understand the spatial distribution of the different scales of heterogeneities and, consequently, influence in obtaining realistic flow scenarios. In this work, an integrated supervised methodology is proposed for the characterization of natural fractures in a low permeability lacustrine carbonate reservoir in Santos basin, Southeastern Brazilian margin. To achieve the objectives of the study, a workflow was developed that involves the actions, briefly described below: (i) descriptive and kinematic analysis at multiple scales of the brittle structures; (ii) understanding of lithological control in the deformation process; (iii) quantification of the deformation in different phases of movement by 2D / 3D structural restoration techniques and (iv) analysis of seismic anisotropy.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.202113316
2021-10-18
2024-04-28
Loading full text...

Full text loading...

References

  1. Caine, J.S., Evans, J.P., Forster, C.B.
    , 1996. Fault zone architecture and permeability structure. Geology24, 1025–1028. https://doi.org/10.1130/0091-7613(1996)024<1025:FZAAPS>2.3.CO;2.
    [Google Scholar]
  2. Downton, J., B.Roure, and L.Hunt
    , 2011, Azimuthal Fourier coefficients: CSEG Recorder, 36, 22–36.
    [Google Scholar]
  3. FOSSEN, H., ROTEVATN, A.
    2016. Fault linkage and relay structures in extensional settings - A review. Earth-Science Reviews. 154, 14–28.
    [Google Scholar]
  4. Hudson, J. A.
    , 1981, Wave speeds and attenuation of elastic waves in material containing cracks: Geophysical Journal of the Royal Astronomical Society, 64, 133–150, doi: 10.1111/j.1365-246X.1981.tb02662.x.
    [Google Scholar]
  5. R. J.Knipe, G.Jones and Q. J.Fisher
    . Geological Society, London, Special Publications, 147, vii–xxi, 1 January 1998, https://doi.org/10.1144/GSL.SP.1998.147.01.01.
    [Google Scholar]
  6. Schoenberg, M.
    , 1980, Elastic behavior across linear slip interfaces: Journal of the Acoustical Society of America, 68, 1516–1521, doi: 10.1121/1.385077.
    [Google Scholar]
  7. WALSH, J.J., BAILEY, W.R., CHILDS, C.
    2003. Formation of segmented normal faults: a 3-D perspective. Journal of Structure Geology, 25, 1251–1262.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.202113316
Loading
/content/papers/10.3997/2214-4609.202113316
Loading

Data & Media 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