Carbonate Reservoir Analysis With Seismic Methods

Seismic Methods For Carbonate Reservoir Analysis

Bandung | 20 – 23 October 2014 | Fee at proposal



This overview of carbonate geology has been presented to several hundred participants in the petroleum industry through the years. It includes a review of carbonate basics (rock and pore types), facies mapping, depositional modeling, diagenetic overprinting, shelf-to-basin profiling, and sequence stratigraphic models. Exploration/production case histories from around the world are presented as examples throughout the course.

The seminar is followed by a field trip to Kepulauan Seribu where living reefs mimic fields that produce from Miocene reservoirs throughout Indonesia. Participants will examine reef, near-reef, and lagoonal settings. The modern facies mapping of this area is based on the analysis of 300 bottom samples and shows definitive patterns of reef distribution. At the end of the field trip, Holocene reef-related facies maps from other areas in the world ocean are presented for comparison.



Who should attend :

  • Managers who have teams working in carbonate settings and those who need an overview of what is important in finding and producing carbonate reservoir.
  • Explorationists, geologists and geophysicists, who need to see the regional perspective of carbonate depositional systems, especially along shelf-to-basin profiles.
  • Production-oriented geologistsand geophysicists who need to know the details of facies variations and how that affects porosity development.
  • Engineers who want a geological summary and understanding of how petrophysics relates to diagenesis and the making or breaking of a reservoir.



What will be learned by participants?

  1.  How to characterize carbonate reservoir and how to put them in perspective
  2. An appreciation of depositional and diagenetic models to predict carbonate reservoir
  3. How to sort out limestones, dolomites, and pore type from a petroleum industry point of view
  4.  How carbonate particles are formed on the seafloor (the field trip) and how modern facies patterns relate to

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