... by clastic rocks that accumulated in the complementary Love Ranch basin. The synorogenic to postorogenic McRae and Love Ranch Formations are as much as 1460 m thick; they filled the Love Ranch basin and onlapped the Rio Grande uplift. Present outcrops of the two formations cover an area of 100 km 2...

... of this event in the region and expand our knowledge of Late Cretaceous to Paleogene tectonism. The McRae Formation marks the onset of deposition in the Laramide Love Ranch Basin, which was located to the northeast of the west-northwest–trending coeval Rio Grande uplift in south-central New Mexico, but its age...

... was, as usual, very good, but timing is everything! Paul was from a ranching family and had always dreamed of owning his own ranch. In 1958, with the royalties from his Wasatch Plateau and Uinta basin discoveries, Paul and his wife Betty bought 1740 acres along the Snake River in Jackson Hole, Wyoming. Several...

.... Basin, Cub Mountain, El Rito, Espinaso, Galisteo, Love Ranch, McRae, Orejon, Palm Park, and San Jose. Although the Blanca Basin, Cub Mountain, El Rito, Espinaso, Love Ranch, McRae, and Orejon Formations are not demonstrably Eocene, their assignment, to that epoch by various workers, past and present...

... the Bighorn Mountains ( Finn et al. , 2010 ). The crust–mantle boundary depth in the region ranges between 40 and 50 km and is typically shallower beneath the north‐northwest‐trending Laramide Bighorn arch and the western edge of the Powder River basin ( Yeck et al. , 2014 ). In the Jacobs Ranch...

... sharp. Near No Wood (southeastern Big Horn Basin), a zone of diastems separates the two. J. D. Love (1939, p. 27) reports an unconformity between the Amsden and Tensleep in the Absaroka Mountains, and Branson and Branson (1941) and Baker (1946) have made similar observations in the Wind River...

...Figure 8. (A) Timing and duration of fracture opening in the Piceance Creek and Love Ranch fields. Burial temperature evolution was adapted for individual fractures based on a temperature history model for the Love Ranch #1 well; see text for details. Range of fluid inclusion T h data...

... the Hunton production which was expected. In C SE¼, Sec. 11, T2N, R20E ( Fig. 1 , no. 12), American Quasar Petroleum drilled the 1–11 Cabe, an unsuccessful test to 15,512 ft TD in Stanley-Jack Fork. The location is in the Potato Hills area of the Ouachita Mountain province. In the Arkoma basin...

.... In west Texas, the primary exploratory success target shifted from the shallower oil-prone plays of the Midland basin back to the deep gas trends of the Delaware and Val Verde basins. The most significant discoveries of 1980 were located in the Loving County area near the New Mexico state line where...

... are part of a group of fossils considered to be of Albian age. If this is correct, the Smoot (upper Gannett unit) must span the Aptian-Albian boundary. The structural pattern of the thrust belt of western Wyoming and southeastern Idaho is very similar to that of the Basin-Range province...

...Thomas L. Holzer; T. Leslie Youd Abstract Excess pore-water pressure and liquefaction at the Wildlife Liquefaction Array in 1987 were caused by deformation associated with both high-frequency strong ground motion and 5.5-second-period Love waves. The Love waves produced large (∼1.5%) cyclic shear...

... and 69 nodal seismometers operated in the vicinity of a 27 km long segment of dark fiber DAS array in the Imperial Valley, Southern California. The study area is a sedimentary basin characterized by intense seismicity and faulting in a transtensional tectonic regime, and hosts multiple producing...