Utah FORGE: 3D Gravity Data
These resources describe the 3D geophysical inversion modeling of gravity data at the FORGE site near Milford, Utah. FORGE is the Frontier Observatory for Research in Geothermal Energy and the site in Utah has been selected by the U.S. Dept. of Energy for a 5-year R&D program to test technologies for the development of Engineered Geothermal Systems (EGS). 3D modelling of gravity data at the FORGE site is to help characterize the subsurface geologic framework. Specifically, modelling of gravity data in 3D, used in conjunction with rock density measurements and other subsurface geologic information can provide an independent test of an existing 3D geologic model (e.g. Witter et al., 2018). Such an exercise can be useful for reducing uncertainty in 3D geologic models (Witter et al, 2019).
Citation Formats
Energy and Geoscience Institute at the University of Utah. (2019). Utah FORGE: 3D Gravity Data [data set]. Retrieved from https://dx.doi.org/10.15121/1542061.
Hardwick, Christian, Witter, Jeff. Utah FORGE: 3D Gravity Data. United States: N.p., 24 Jun, 2019. Web. doi: 10.15121/1542061.
Hardwick, Christian, Witter, Jeff. Utah FORGE: 3D Gravity Data. United States. https://dx.doi.org/10.15121/1542061
Hardwick, Christian, Witter, Jeff. 2019. "Utah FORGE: 3D Gravity Data". United States. https://dx.doi.org/10.15121/1542061. https://gdr.openei.org/submissions/1144.
@div{oedi_3796, title = {Utah FORGE: 3D Gravity Data}, author = {Hardwick, Christian, Witter, Jeff.}, abstractNote = {These resources describe the 3D geophysical inversion modeling of gravity data at the FORGE site near Milford, Utah. FORGE is the Frontier Observatory for Research in Geothermal Energy and the site in Utah has been selected by the U.S. Dept. of Energy for a 5-year R&D program to test technologies for the development of Engineered Geothermal Systems (EGS). 3D modelling of gravity data at the FORGE site is to help characterize the subsurface geologic framework. Specifically, modelling of gravity data in 3D, used in conjunction with rock density measurements and other subsurface geologic information can provide an independent test of an existing 3D geologic model (e.g. Witter et al., 2018). Such an exercise can be useful for reducing uncertainty in 3D geologic models (Witter et al, 2019).}, doi = {10.15121/1542061}, url = {https://gdr.openei.org/submissions/1144}, journal = {}, number = , volume = , place = {United States}, year = {2019}, month = {06}}
https://dx.doi.org/10.15121/1542061
Details
Data from Jun 24, 2019
Last updated Mar 9, 2020
Submitted Jun 24, 2019
Organization
Energy and Geoscience Institute at the University of Utah
Contact
Greg Nash
801.585.9986
Authors
Original Source
https://gdr.openei.org/submissions/1144Research Areas
Keywords
geothermal, energy, Utah FORGE, 3D gravity data, gravity data, Utah Forge gravity data, Utah geothermal, complete bouguer, density model, gravity, terrestrial gravity survey, observed gravity, FORGE, geophysics, 3D, 3D model, 3D gravity, gravity anomaly, EGS, MilFord, inversion, modelling, inverse, Roosevelt Hot Springs, bouger, top of granite, density, survey, simple bouger, free air, terrain correction, geologic, correction, corrected, Utah, model, modelingDOE Project Details
Project Name Utah FORGE
Project Lead Lauren Boyd
Project Number EE0007080