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February 2008 - Rocky Mountain Association of Geologists

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Friday Luncheon Programs<br />

It is also critical to characterize these plays on a regional scale utilizing both the<br />

techniques <strong>of</strong> Play Fairway Analysis (PFA) coupled with conventional Hydrocarbon<br />

System Analysis. The techniques <strong>of</strong> Hydrocarbon System Analysis along with routine<br />

geochemical and geologic analysis provide the spatial input for the PFA. The PFA<br />

focuses on the construction <strong>of</strong> common risk segment maps which indicate the proper<br />

relative probability for accumulation. These relative common risk segments maps are<br />

combined with measures <strong>of</strong> the data quantity and confidence to construct absolute<br />

probability maps that form the basis for a spatial probability <strong>of</strong> geologic success<br />

(Pg). Finally, the Pg maps are combined with representations <strong>of</strong> the infrastructure<br />

in order to access the probability <strong>of</strong> commercial success.<br />

This talk will illustrate the techniques <strong>of</strong> Hydrocarbon System Analysis and<br />

Play Fairway Analysis with two case studies that led to exploration focus and the<br />

acquisition <strong>of</strong> leases.<br />

Hovenweep-Ismay Petroleum System, Blanding<br />

Sub-basin <strong>of</strong> the Paradox Basin, Utah<br />

<strong>February</strong> 15<br />

By Edward B. Coalson, Coyote Oil & Gas Company, LLC, Conifer, Colorado, and Harvey<br />

R. DuChene, 2HNK Energy, LLC, Lake City, Colorado<br />

Oil and gas in<br />

the Blanding<br />

sub-basin are<br />

produced mainly<br />

from upper Ismay<br />

(Desmoinesian)<br />

carbonate mounds.<br />

In this presentation we will cover aspects <strong>of</strong> the Hovenweep-Ismay (!) petroleum<br />

system in the Blanding sub-basin <strong>of</strong> the Paradox Basin. Regionally, pore fluids in the<br />

Ismay and Desert Creek zones <strong>of</strong> the Paradox Formation follow trends consistent<br />

with the type and maturity indicators <strong>of</strong> organic material, and seem to reflect mainly<br />

Laramide burial. Basinward (northeast) <strong>of</strong> the Blanding sub-basin, Ismay and Desert<br />

Creek hydrocarbons are dominantly natural gas with very little mobile water. This part<br />

<strong>of</strong> the basin is currently seeing a play for “resource-type” natural gas accumulations<br />

in the Gothic Shale, which we will discuss briefly on the basis <strong>of</strong> rumor and innuendo.<br />

Shelfward (southwest) <strong>of</strong> the Blanding sub-basin, Ismay and Desert Creek pore fluids<br />

consist <strong>of</strong> oil with associated gas and significant producible water. In the Blanding<br />

Basin itself, pore fluids are mainly oil and associated gas, with relatively little mobile<br />

formation water. These patterns meet our criteria for a “basin-bottom” system.<br />

Oil and gas in the Blanding sub-basin are produced mainly from upper Ismay<br />

(Desmoinesian) carbonate mounds. The mounds form linear, subparallel trends; are<br />

immediately underlain by thickened sections <strong>of</strong> Hovenweep Shale; are flanked by thick<br />

salina anhydrites; and are immediately overlain by thin upper Ismay sabkha deposits<br />

and marine carbonates <strong>of</strong> the basal Honaker Trail Formation. Correlative, but thinner,<br />

marine-shelf upper Ismay carbonates are underlain by thin Hovenweep Shale.<br />

Based mainly on mapping <strong>of</strong> these thickness trends and on serial stratigraphic<br />

cross sections, we propose that the anomalously thick, productive upper Ismay<br />

Continued on page 30 »<br />

OUTCROP<br />

29<br />

www.rmag.org

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