About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
Rocky Mountain Association of Geologists
Abstract
Hamilton Creek Field
Abstract
Production from the Hamilton Creek Field, San Miguel Co, Colorado is the result of interbedded source rocks, reservoirs, and seals that have been folded and faulted into a three-way fault-bound closure, with the Hamilton Creek “B” Fault acting as the primary lateral seal. All pay is located in the footwall of this fault. Cyclic Pennsylvanian marine sedimentation stratifies organic-rich dolomitic shales with chlorite-rich sands, limestones, dolomites, and anhydrites. Fluvio-deltaic sands sourced from the rising Uncompahgre/San Luis Uplift to the northeast spread in pulses across the Hamilton Creek area. Principle production from the field comes from these sands. Structural elevation and reservoir quality are dominant controls on per-well production.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
Watermarked PDF Document: $14 | |
Open PDF Document: $24 |