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- W2314903902 abstract "As part of an effort to understand a complicated shallow lowtemperature geothermal system in the Arkansas Valley, Colorado, we focused on Chalk Cliff Valley by acquiring a 3-D seismic data with a 240 m2 footprint. In order to optimize a reflection image of the site, we use refraction and wavefield modeling in an initial attempt to interpret the shot gathers. Our results show the bedrock dipping to the south by up to 31◦, up to 110 m deep at the southern extent of the site. We also find a water table depth of 10 m and present evidence that the saturated sediments are terminating near the northern end of the site where the bedrock is shallowing. We also find that the velocity field may be anisotropic with the refraction model results estimating a 12 percent increase in the N-S direction. Our findings, and particularly the fractured bedrock and a termination of the saturated sediments on the northern end of our study area are consistent with geologic observations and SelfPotential data identifying a localized anomaly associated with up-welling (hot) water. The velocity model will guide reflection imaging to be performed shortly." @default.
- W2314903902 created "2016-06-24" @default.
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- W2314903902 date "2010-01-01" @default.
- W2314903902 modified "2023-09-26" @default.
- W2314903902 title "Preliminary results for a near surface 3‐D seismic survey of a geothermal system in Colorado" @default.
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- W2314903902 doi "https://doi.org/10.1190/1.3513228" @default.
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