• Geology
  • Published 2011

Sequence-Stratigraphic Controls on Reservoir-Scale Architecture of the Middle Mesaverde Group, Douglas Creek Arch, Colorado

@inproceedings{Hlava2011SequenceStratigraphicCO,
  title={Sequence-Stratigraphic Controls on Reservoir-Scale Architecture of the Middle Mesaverde Group, Douglas Creek Arch, Colorado},
  author={Kimberly Sue Hlava},
  year={2011}
}
Hlava, Kimberly Sue (M.S., Geology [Department of Geological Sciences]) Sequence-stratigraphic controls on reservoir-scale architecture of the middle Mesaverde Group, Douglas Creek Arch, Colorado Thesis directed by Associate Professor Matthew J. Pranter The middle Mesaverde Group of the Douglas Creek Arch, northwestern Colorado, is represented by a complex succession of fluvial to marine strata that serve as outcrop analogs to laterally equivalent natural gas reservoirs in the Piceance and… CONTINUE READING
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References

Publications referenced by this paper.
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Using the ideas outlined in Allen and Posamentier (1993), the interval would be one full sequence

The present study interval has many similarities with Allen, Posamentier
  • Strata above B-1 (CP1, high N:G) would form the amalgamated fluvial sandstone bodies of the ELST and LLST. Overlying this unit would be the transgressive surface and estuarine and coastal-plain strata of the TST. The
  • 1993
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HIGHLY INFLUENTIAL

The boundary between S4-4 and S4-5

Kirschbaum, Hettinger
  • 2004
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HIGHLY INFLUENTIAL

Parasequences are relatively conformable successions of genetically

Shanley, McCabe
  • 1994
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HIGHLY INFLUENTIAL

Above 323 ft (98.5 m), the study interval is equivalent

Brownfield, Johnson
  • 2008
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HIGHLY INFLUENTIAL

The study interval (red bar) with respect to the Iles clastic wedge as described by Crabaugh

L Fig
  • Modified from Crabaugh
  • 2001
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HIGHLY INFLUENTIAL