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GEOMARK CASE STUDY
Case Studies in the Integration of Rock and Fluid
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Objective
Provide case studies in which rock and fluid integration and application are shared and given as examples for the industry to them execute, as well.
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Business Impact
Unlocks the integration power and potential for subsurface investigators, showing why and how rock and fluid interact, providing insight into determining play viability and making business-critical decisions.
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Interpretation
The geochemistry-petrophysics data showed that:
- Distinct geochemical fluid ratios correlate to stratigraphic benches within the Bone Spring and Wolfcamp formations stratigraphy.
- Petrophysical properties combined with the geochemical fluid variance highlights the generative organic-enriched stratigraphy versus the charged tight siltstones; as well as what and where the generated and expelled hydrocarbons migrated locally and regionally.
- Increased total porosity and permeability in the Wolfcamp XY correlates to charge from the underlying WFMP A.
- The WFMP is an organically-enriched, lower porosity, HC-filled zone with distinct geochemical fluid signatures.
- The WFMP B is an organically-lean, higher clay volume, mixed water, and HC-filled zone. The total porosity is dominated by micropores associated with clay volume. The fluid signature in these clay-prone turbidites is differentiable.
- The distinct signature changed in ratios between the WFMP B versus A benches. Those families can then be used to interpret what migrated and charged the WFMP XY and Bone Spring 3 sandstone intervals.
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