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Abstract: Missing Stratigraphic Sections in Tertiary Sandstone Reservoirs of the Gulf Coast: Faults or Unconformities and Implications for Development Strategies
R P. Major (1), R. Dean Johnstone (2)
Missing section identified by log correlation in Gulf Coast boreholes is typically interpreted as displacement by downward movement along the upper surface of a growth fault. A common interpretation strategy is to link wells containing missing section with a growth fault having a curvilinear geometry in map view. We present here an alternative possibility: section missing because of erosion. This interpretation has a very different geometry and results in alternative implications for compartmentalization in stacked sandstone/shale reservoirs.
Missing stratigraphic section in the F39 Frio reservoir of Lavaca Bay field, an Oligocene barrier/strandplain reservoir in Calhoun County, Texas, has been attributed to growth faulting. The geometry of missing sections in wells in this reservoir is complex, however, and the standard fault interpretation results in an unusual and geologically unlikely structural configuration. A dipmeter log from a key well in this reservoir indicates a sharp boundary at the depth of missing section and a distinct change in northwest dip from 8° above to 14° below. The map-view geometry of missing section defines two subcircular areas of erosion. These features are interpreted to have formed by local uplift due to shale diapirism and concomitant erosion of an overlying sandstone, which was deposited as a widespread tabular strandplain. The current structural crest of the field occurs between the two eroded paleohighs. Two wells in the present structural crest penetrated thick reservoir sandstone and have yielded approximately 20 percent of the cumulative production from this reservoir.
Distinguishing missing section caused by erosional unconformities from that caused by growth faulting has three implications for reservoir development and resource assessment: (1) compartments bounded by faults can contain sandstones of nearly uniform reservoir properties throughout, whereas compartments caused by erosion will contain thin sandstones along the margins, (2) interpreting compartment boundaries as faults will result in very different compartment shapes than would result from the unconformity interpretation, and (3) misinterpreting missing section can lead to miscorrelation of productive zones in stacked reservoirs and, thus, to incorrect estimations of remaining resources.
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ACKNOWLEDGMENTS AND ASSOCIATED FOOTNOTES
(1) Bureau of Economic Geology, The University of Texas at Austin, Austin, TX 78713
(2) Neuman Production Co., P.O. Box 769, Point Comfort, TX 77978
Copyright © 1999 by The Gulf Coast Association of Geological Societies