--> Surface to Subsurface Correlation of the Late Ordovician Montoya Group, southern New Mexico and western Texas, by M.C. Pope, H. Liu, D.Thomas, #90025 (2004)
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Surface to Subsurface Correlation of the Late Ordovician Montoya Group, southern New Mexico and western Texas

POPE, MICHAEL C., Washington State University, Department of Geology, Pullman, WA 99164, HUAIBO LIU, and DAVE THOMAS, Tom Brown, Inc., Midland, TX, 79702

A field-based Previous HitsequenceNext Hit stratigraphic framework including hand-held gamma-ray profiles of the Late Ordovician Montoya Group in southern New Mexico and western Texas was correlated into the subsurface using wireline logs, and core/cuttings descriptions. This Previous HitanalysisNext Hit indicates that 2nd- and 3rd-order depositional sequences are regionally traceable. In outcrop the Montoya Group rests unconformably on the Early Ordovician El Paso Group, but in the subsurface it lies unconformably on the Middle Ordovician Simpson Group. The 2nd-order TST is characterized by skeletal packstones/wackestones with lower gamma-ray values. Deepwater cherty facies with relatively higher gamma-ray values, characterize the 2nd-order maximum flooding zone. The 2nd-order HST is composed of subtidal carbonates shallowing upward into prograding peritidal carbonate facies; this unit has a higher gamma ray response at its base and lower values at its top. In the subsurface the top of the Montoya Group may be Previous HitwellNext Hit-cemented ooid grainstone. The 2nd-order Previous HitsequenceNext Hit boundary separating the Montoya Group from the overlying Fusselman Dolomite is a subaerial surface in outcrop but is conformable in the subsurface. Montoya outcrops can be differentiated into six 3rd-order sequences. Previous HitSequenceNext Hit 0 is locally present within incised valleys or topographic lows on the underlying El Paso karst surface. Previous HitSequenceNext Hit 5 occurs only far down dip being eroded up dip. Sequences 2-4 are regionally recognizable and correlative into the subsurface. These sequences are equivalent to the Cable Canyon Sandstone (0 and 1), Upham Formation (1), lower Aleman Formation (2), upper Aleman Formation (3), and Cutter Formations (4 and 5) respectively. Integrating field observations, hand-held gamma-ray Previous HitlogNext Hit profiles and subsurface data provides a detailed Previous HitsequenceTop stratigraphic framework to exploit the unusual Montoya Group chert reservoir.