2 Unraveling the Tertiary Stratigraphy and Structure of the Pacific Northwest and Its Implications for Hydrocarbon Occurrence and Underground Gas Storage: In Honor of Alan and Wendy Niem
Monday, 13 May 2002
8:00 AM - 12:00 PM
DEPOSITIONAL MODEL FOR EOCENE AND OLIGOCENE SANDSTONES IN THE GRAYS HARBOR BASIN, WASHINGTON STATE
Paper number: 2-8
Program: THEME SESSIONS
Time: 9:40 AM – 9:55 AM
Authors
Abstract
A depositional model for Eocene and Oligocene sedimentation in the GHB has been developed from outcrop studies, well and seismic data. Deltaic sandstones, eroded during sea level lowstands, were reworked and carried westward by fluvial systems originating in the Puget and Chehalis Basins. Fluvial systems fed submarine canyons located between basement highs which, in turn, fed submarine fan systems in the GHB. At least four distinct episodes of submarine fan sedimentation are recognized in the GHB. Two submarine fan sandstones, the Basal Cowlitz and Basal Lincoln Creek sandstones, appear to be correlative the productive Clark & Wilson Sandstone at Mist Field and the Zone 2 sandstone reservoir at Jackson Prairie Gas Storage Field.