...Figure 6. —(A) Structure map, contoured on Kinder-hookian shale, Glick field. (B) Isopach map, top of productive chat reservoir, Glick field. From Rogers et al. (1995) . ...

... on Dollarhide field's chert reservoirs in west Texas. Another interesting article is our work on the spiculitic Mississippian "chat" reservoir at Glick field in Kansas ( Rogers et al., 1995 ). The unusual spicule-rich cherts that form the reservoir for the 400 bcf Glick field helped provide a catalyst...

...Figure 9 Scanning electron microscope (SEM) photograph of chat sample from Shell 1-36 Robbins in Glick field at 4856 ft (1480 m) showing corroded quartz crystals and microporosity. Scale bar is 10 μm. ...

...Figure 1 (A) Regional post-late Mississippian tectonic elements, and in green, some of the larger oil or gas fields that produce from Mississippian chert (including chat) and/or spiculite in central Kansas. Bindley, Schaben, and Glick fields are specifically discussed in the text. The subsurface...

... that the Joachim, Plattin, Kimmswick, and Fernvale formations are all separated, one from another, by unconformities. However, subsequent authors ( McKnight, 1935 ; Frezon and Glick, 1959 ) reported that physical evidence for these breaks is obscure. With additional reading and limited field observations I became...

... of more highly soluble siliceous organisms, such as sponges, is the most likely source of silica for the chat. Sponge bioherms were prevalent in some Paleozoic seas, and sponge spicules in such bioherms are believed to be the source of silica in the chat at Glick field in Kansas ( Rogers et al., 1995...

...Ernest E. Glick Abstract Prior to about 1974, most of the work in the Mississippi embayment area by members of the U.S. Geological Survey was motivated by interest in the embayment’s paleontologic aspects, stratigraphy, and economic resources, especially ground water. However, an excellent...

... explanations have been offered for the diverse trends of faults in northern Arkansas. Glick (1997) attributed diverse structural trends to differential solution and compaction over paleotopography in the Precambrian basement. Ancillary to their discussion of foreland flexure in the Arkoma basin, Bradley...

... of sandstone, limestone, and dolomite ( Fig. 4 ). The formation ranges in thickness from 350 ft in the west to 650 ft in the east. It is divisible into seven members that are lithologically distinctive and objectively definable in the field. Four of these members are “formal” and have been proposed by earlier...

... for suggesting this problem and for their direction throughout its investigation. The Arkansas Geological Commission provided funds for field expenses. © 1968 American Association of Petroleum Geologists. All rights reserved 1968 American Association of Petroleum Geologists The purpose...

... relation to seismicity , U.S. Geol. Surv. Misc. Field Studies Map, MF-914 , scale 1:1,000,000. Hildenbrand , T.G. , R.P. Kucks , M.F. Kane , and J.D. Hendricks ( 1979 ). Aeromagnetic map and associated depth map of the upper Mississippi embayment region , U.S. Geol. Surv. Misc...