Anadarko basin

Vertical Land Motion of the High Plains Aquifer Region of the United States: Effect of Aquifer Confinement Style, Climate Variability, and Anthropogenic Activity

“…Total volume of water removed in the High Plains aquifer is estimated at 330 km 3 as of 2007 (Scanlon et al., 2012). By comparison, cumulative oil production in the nearby Anadarko Basin is estimated at more than 0.8 km 3 (Davis et al., 1988) while the Permian Basin to the south has produced over 5.25 km 3 (US Energy Information Administration, 2018), meaning widespread uplift due to oil production and associated byproducts is highly unlikely. There are no geologic indicators of recent large magnitude (>M6) tectonic activity or magmatic activity (Gutentag et al., 1984) near the center of uplift that can impact vertical motions (e.g., post‐seismic relaxation; Gourmelen & Amelung, 2005; Hammond et al., 2012) or mantle upwelling (Kreemer et al., 2020).…”

Magnetotelluric Imaging of the Lithospheric Structure of the Southern Oklahoma Aulacogen: Evidence for Long‐Term Weakening Caused by Rifting

“…The resistivity of both layers was permitted to vary as the inversion proceeded (Figure S7b in Supporting Information S1). The basin depths were taken from seismic, drilling and isopach data from Laske et al (2013), Perry (1989), Davis et al (1988), andBrewer et al (1983). The resulting inversion model is shown in Figure 4.…”

Correction for distortion in polarization of reflected shear‐waves in isotropic and anisotropic media

“…Compiled primarily from Cipriani (1963), Hills and Kottlowski (1983), Mankin (1986). Other sources are Amsden (1979Amsden ( , 1980Amsden ( , 1989, Amsden and Sweet (1983), Johnson (1988), Hester and others (1990), Baars and others (1991), Carpenter and Evans (1991), Davis and Northcutt (1991), Wilson and others (1991), Knode and others (1993).…”

“…Hills and Kottlowski (1983), Mankin (1986). Other sources are Amsden (1979Amsden ( , 1980Amsden ( , 1989, Amsden and Sweet (1983), Johnson (1988), Hester andothers (1990), Baars and others (1991), Carpenter and Evans (1991), Davis and Northcutt (1991), Wilson and others (1991), Knode and others (1993 Figure 36.B: Time delay between fast and slow split shear waves from analysis of the Brady Ranch 1-5 VSP data. The dashed curve is the result of applying Synchronous Rotation at each depth level, and the solid curve is the result of applying downward continuation plus SR.…”