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Permian paleogeography Delaware and Midland Basins
Permian Basin Precambrian structure
Bone Spring depositional systems
Delaware Basin gas + oil windows
Lea County, New Mexico
Delaware Basin Bone Spring + Wolfcamp stratigraphy
Bone Spring 2 type log with GT 8 percent porosity isopach shaded yellow
Bone Spring 2 GT 8 percent log porosity isopach Lea Co NM, 21-26S and 32-36E
Bone Spring log + cored reservoir interval
Bone Spring cored reservoir porosity vs permeability
Conclusions
• Paleogeography studies indicate highlands to the N (ancestral Rockies), W
(Diablo platform), E (Central Basin Platform) and S (Marathons) served as
potential source areas for the Delaware Basin Bone Spring and Wolfcamp.
• Bone Spring 2 higher initial rates and higher estimated ultimate recoveries
correlate with thicker log porosity isopach areas above 8 percent porosity. Core
data supports higher core permeability with higher log porosity.
• Detailed log correlation and mapping of Bone Spring 2 log porosity defines the
production sweet spots for offset infill drilling.
• Bone Spring 2 porosity thick trends oriented from NE-SW indicate cross bedded
channel sand deposition sourced from structural highlands to the N, E and W.
• Porosity logs in pilot holes or older wells that tested deeper structures are
crucial for mapping the porosity thick trends within the Bone Spring 2 and
maximizing the Bone Spring 2 play economics.

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Bone Spring 2 porosity distribution in Lea Co New Mexico.pdf

  • 1. Permian paleogeography Delaware and Midland Basins
  • 4. Delaware Basin gas + oil windows Lea County, New Mexico
  • 5. Delaware Basin Bone Spring + Wolfcamp stratigraphy
  • 6. Bone Spring 2 type log with GT 8 percent porosity isopach shaded yellow
  • 7. Bone Spring 2 GT 8 percent log porosity isopach Lea Co NM, 21-26S and 32-36E
  • 8. Bone Spring log + cored reservoir interval
  • 9. Bone Spring cored reservoir porosity vs permeability
  • 10. Conclusions • Paleogeography studies indicate highlands to the N (ancestral Rockies), W (Diablo platform), E (Central Basin Platform) and S (Marathons) served as potential source areas for the Delaware Basin Bone Spring and Wolfcamp. • Bone Spring 2 higher initial rates and higher estimated ultimate recoveries correlate with thicker log porosity isopach areas above 8 percent porosity. Core data supports higher core permeability with higher log porosity. • Detailed log correlation and mapping of Bone Spring 2 log porosity defines the production sweet spots for offset infill drilling. • Bone Spring 2 porosity thick trends oriented from NE-SW indicate cross bedded channel sand deposition sourced from structural highlands to the N, E and W. • Porosity logs in pilot holes or older wells that tested deeper structures are crucial for mapping the porosity thick trends within the Bone Spring 2 and maximizing the Bone Spring 2 play economics.