Geologic and structure contour map of the Clay Basin gas field and vicinity, Daggett County, Utah, and Sweetwater County, Wyoming

1945 ◽  
Author(s):  
C.E. Dobbin ◽  
Robert Davison

1945 ◽  
Author(s):  
C.E. Dobbin ◽  
R. Davidson
Keyword(s):  




Geophysics ◽  
1954 ◽  
Vol 19 (3) ◽  
pp. 509-516 ◽  
Author(s):  
Wallace L. Matjasic

The discovery well of the Wild Goose gas field was drilled and completed in 1951 on a structure located by a reflection seismograph survey conducted in 1950. An additional seismograph survey was made subsequent to discovery to define the structure better for further development. The illustrations include two seismic cross sections, a contour map based on the original seismic reflection data, an aeromagnetic map, a structure contour map, and an electric log of the discovery well. The producing sands are in an interval between the Forbes shale of Upper Cretaceous age and the overlying Capay shale of Eocene age.



1940 ◽  
Author(s):  
W.B. Kramer ◽  
G.G. Frasier ◽  
R. McMillan ◽  
J.G. Cox


Geophysics ◽  
1961 ◽  
Vol 26 (6) ◽  
pp. 673-681
Author(s):  
John H. Earl ◽  
John N. Dahm

Desert Springs Area is located in central Sweetwater County, Wyoming, on the west flank of the Red Desert Basin, with the Rock Springs uplift to the west and the Wamsutter arch to the south. The producing reservoirs are in the Upper Cretaceous Lewis and Almond formations, with the Almond being the uppermost formation of the Mesaverde Group in the area. Petty Geophysical Engineering Company was contracted to conduct a seismic survey over the area. Work was initiated on April 3, 1956 and completed July 24, 1956. Fault evidence was noted in the area, based on discontinuity of seismic events and change of reflection characteristics. On the basis of this fault evidence, El Paso Natural Gas Company drilled the Desert Springs No. 1 well which potentialed for 7.7 million cubic feet of gas per day. This led to additional drilling; and, as of January 1959, eight wells have found production at an average depth of 6,100 ft, having potentials from 7.7 million cubic ft of gas per day with some distillate. A detailed study of stratigraphy, lithology, and sedimentation, along with a detailed review of the seismic data utilizing the velocity survey in Desert Springs No. 1 well, was undertaken. The final analysis revealed that the phenomena originally mapped as a fault is in reality a series of facies changes. Three main stratigraphic type traps: offshore bar, lateral facies change, and wedge‐out below an unconformity; are believed to be present in this area, thus making an integrated and coordinated exploration program between the geologists and the geophysicist necessary if we expect to find additional oil and gas reservoirs of this nature.



Author(s):  
Keinosuke Kobayashi

Equidensitometry as developed by E. Lau and W. Krug has been little used in the analysis of ordinary electron photomicrographs, yet its application to the high voltage electron images proves merits of this procedure. Proper sets (families) of equidensities as shown in the next page are able to reveal the contour map of mass thickness distribution in thick noncrystalline specimens. The change in density of the electron micrograph is directly related to the mass thickness of corresponding area in the specimen, because of the linear response of photographic emulsions to electrons and the logarithmic relation between electron opacity and mass thickness of amorphous object.This linearity is verified by equidensitometry of a spherical solid object as shown in Fig. 1a. The object is a large (1 μ) homogeneous particle of polystyrene. Fig. 1b is a composite print of three equidensities of the 1st order prepared from Fig. 1a.



2011 ◽  
Author(s):  
Marie Aschehoug ◽  
C. Shah Kabir
Keyword(s):  


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