Gpr Attribute Analysis

Lemke, Seth R.; Mankowski, Leonard C.

doi:10.3997/2214-4609-pdb.200.2000_032

13th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems 2000

DOI: 10.3997/2214-4609-pdb.200.2000_032

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Gpr Attribute Analysis

Seth R. Lemke¹,

Leonard C. Mankowski²

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2007

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Three-dimensional facies architecture and three-dimensional calcite concretion distributions in a tide-influenced delta front, Wall Creek Member, Frontier Formation, Wyoming

Lee¹,

Gani²,

McMechan³

et al. 2007

Bulletin

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Cluster analysis of the GPR attributes (instantaneous amplitudes and wave numbers) calibrated with the cores and the outcrop was used to predict the distribution of near-zero permeability concretions throughout the 3-D GPR volume; clusters of predictive attributes were defined and applied separately in the bars and channels. The predicted concretions in the bars and the channels are 14.7 and 10.2% by volume, respectively, which is consistent with those observed in the cores (14.7 and 10.5%, respectively), and their shape and thickness are also generally in consonance with those in the outcrop and cores. The estimated concretions are distributed in an aggregate pattern with irregularly shaped branches within the 3-D GPR volume, indicating that the cementation does not follow a traditional center-to-margin pattern. The concretions and 3-D geological solid model provide cemented flow baffles and a 3-D structural framework for 3-D reservoir modeling, respectively.

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Three-dimensional facies architecture and three-dimensional calcite concretion distributions in a tide-influenced delta front, Wall Creek Member, Frontier Formation, Wyoming

Lee¹,

Gani²,

McMechan³

et al. 2007

Bulletin

View full text Add to dashboard Cite

show abstract

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Gpr Attribute Analysis

Cited by 1 publication

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Three-dimensional facies architecture and three-dimensional calcite concretion distributions in a tide-influenced delta front, Wall Creek Member, Frontier Formation, Wyoming

Three-dimensional facies architecture and three-dimensional calcite concretion distributions in a tide-influenced delta front, Wall Creek Member, Frontier Formation, Wyoming

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