37. If the material below the sandstone of problem 26 is a shale with E=31.2 x 109 N/m, Poisson\'s Ratio 0.3, and a density of 2650 kg/m3, what is the reflection coefficient of the interface between the shale and sandstone?? a. 0.078 b. -0.225 c. -0.311 d. 0.179 e. None of the above 38. What is the most common well type used to produce natural gas from the Barnett Shale at DFW Airport? a. Vertical wells b. Disposal wells c. Individual horizontal wells d. Multiple horizontal wells from a single drilling pad e. None of the above 39. Why is fracking necessary to produce natural gas from the Barnett Shale in the DFW area? a. b. c. d. e. Fracturing breaks the Barnett Shale seal providing access to sandstone reservoir Fracturing reduces the permeability of the Barnett Shale Fracturing increases the permeability of the Barnett Shale Fracturing permits the natural gas to be absorbed in the fracking fluids None of the above 40. What is the source rock in the East Texas Oil Field? a. b. c. d. e. Barnett Shale Morrison Formation Eagle Ford Shale Woodbine Sandstone None of the above 41. Which of the following describes processes that formed Guadalupe Peak in West Texas? a. b. c. d. Formed by deposition of sediments rich in calcite Tectonic activity has been minimal in the area during the past 20 my The limestone was precipitated from sea water by marine organisms None of the above Solution 40.EAGLE FORD SHALE: The Eagle Ford is a geological formation directly beneath the Austin Chalk. It is considered to be the \"source rock\", or the original source of hydrocarbons that are contained in the Austin Chalk above it. The formation was penetrated many times as operators targeted the Edwards Limestone formation along the Edwards Reef Trend. The formation is best known for producing variable amounts of dry gas, wet gas, NGLs, condensate and oil. The most active area lies above the Edwards Reef Trend where the formation yields a gas-condensate production stream. Unlike many other shale plays, it does not exhibit natural fracturing within the formation. 41.d The Permian period of geologic time occurred from 251 to 299 million years ago. The earth had already seen life diversify from simple, primitive forms such as algae and fungi to amphibians, fishes, and insects. The earth\'s surface had also been evolving and shifting. Thin plates of crust moved constantly over the softer material below, steadily changing the position of the continents. Through much of the early and middle Permian all of the continents were joined together, forming the supercontinent of Pangea. Much of modern-day New Mexico and Texas occupied the western edge of this enormous landmass near the equator. A vast ocean surrounded Pangea, but a narrow inlet, the Hovey Channel, connected the ocean with the Permian Basin, an inland sea which covered parts of what is now northern Mexico and the southwestern United States. The Permian Basin had three arms: the Marfa, Delaware, and Midland Basins. The .