--> ABSTRACT: Sequence Stratigraphy of the Permian Delaware Mountain Group, Basin Floor Setting, Delaware Basin, West Texas and Southeastern New Mexico: Application of Stacking Pattern Analysis, by Wade D. Hutchings; #90906(2001)
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Wade D Hutchings1

(1) Marathon Oil Company, Houston, TX

ABSTRACT: Sequence Stratigraphy of the Permian Delaware Mountain Group, Basin Floor Setting, Delaware Basin, West Texas and Southeastern New Mexico: Application of Previous HitStackingNext Hit Pattern Analysis

The Permian Delaware Mountain Group (DMG) consists of cyclic packages of sandstone, siltstone, carbonate mudstone, and organic-rich siltstone that were deposited in the Delaware Basin during Guadalupian time. Three orders of stratigraphic cyclicity are recognized in the DMG: eight low-order cycles, 32 intermediate-order cycles, and more than 50 high-order cycles. Low and intermediate-order cycles are similar in scale to composite and high-frequency sequences. All cycles are bounded by organic-rich siltstones or carbonate mudstones that represent periods of sediment starvation in the basin.

Previous HitStackingNext Hit pattern analysis combined with other stratigraphic tools can be effectively used in the unlimited-accommodation setting of the DMG. High-frequency cyclicity is better expressed in the distal, basin-floor setting of the Delaware Basin due to more complete stratal preservation than in proximal, slope settings. A one-dimensional stratigraphic framework from the basin center correlates over long distances in the northern Delaware Basin.

Regional correlation of low-order cycles characterized by upward-thinning cycle Previous HitstackingNext Hit patterns identifies a dynamic depositional system that is linked closely to stratigraphic position within low and intermediate-order cycles. In most low-order cycles, basal intermediate-order cycles thicken basinward and upper cycles thicken slopeward in response to changing accommodation conditions on the coeval carbonate shelf.

Correlation of several limestone intervals to the PDB-04 core and the Guadalupe Mountains aid in allowing a comparison between low-order cycles from the basin and composite sequences from the shelf. This comparison supports reciprocal sedimentation concepts at several orders, and combined with basin-restricted cross-sections documents a high degree of stratigraphic organization for the DMG.

AAPG Search and Discovery Article #90906©2001 AAPG Annual Convention, Denver, Colorado