C. A. Kaye
1959, Professional Paper 317-B
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Publication Extents
Not all publications have extents, not all extents are completely accurateC. A. Kaye
1959, Professional Paper 317-A
No abstract available....
Verl R. Wilmarth
1959, Bulletin 1087-A
Ray E. Wilcox
1959, Bulletin 1028-N
No abstract available....
G. E. Harbeck Jr., G. E. Koberg, G.H. Hughes
1959, Professional Paper 272-B
J.T. Hack, R.S. Young
1959, Professional Paper 354-A
Dorothy Carroll
1959, Professional Paper 314-F
E.L. Hamilton, R.W. Rex
1959, Professional Paper 260-W
L. R. Stieff, T. W. Stern, Seiki Oshiro, F. E. Senftle
1959, Professional Paper 334-A
R. W. Imlay
1959, Professional Paper 314-G
S. E. Frezon, E.E. Glick
1959, Professional Paper 314-H
E.B. Eckel, Charles Milton, P.T. Sulsona
1959, Professional Paper 327
Philip T. Stafford
1959, Professional Paper 315-A
The subsurface Horseshoe atoll is an arcuate accumulation of fossiliferous limestone 70 to 90 miles across in the northern part of the Midland basin, in western Texas. The stratigraphy, the lithologic character of the rocks, and the petroleum reservoirs of the southeastern part of the atoll in Scurry County and...
Irving Jerome Witkind
1959, Bulletin 1073
No abstract available....
R. J. Burnside
1959, Professional Paper 315-B
The Horseshoe atoll is an arcuate mass of deeply buried fossiliferous limestone of Pennsylvanian and early Permian age in the Midland basin of west Texas. The southern part of the atoll is in southern Borden and northern Howard Counties. From early Strawn until early Wolf camp time this atoll, which...
P.E. Byerly, H.R. Joesting
1959, Professional Paper 316-C
No abstract available....
Wilbert H. Hass
1959, Professional Paper 294-J
The Chappel limestone of Early Mississippian (late Kinderhook and probably partly early Osage) age crops out in the Llano region of Texas where it is as much as 45 feet thick. It contains three conodont faunal zones which, from youngest to oldest, are herein designated: (1) the Bactrognathus communis zone...
Clyde P. Ross, Richard Rezak
1959, Professional Paper 294-K
The story of Glacier National Park begins about 500 million years ago, at a time when there were no mountains in the region - only a vast, exceedingly shallow sea, bordered by desolate plains. The sand, clay, and mud, in part very limy, that were laid down in this sea...
R. J. Ross Jr.
1959, Professional Paper 294-L
J.B. Mertie Jr.
1959, Professional Paper 314-E
V.E. McKelvey, James S. Williams, R. P. Sheldon, E. R. Cressman, T. M. Cheney, R. W. Swanson
1959, Professional Paper 313-A
No abstract available....
Clyde P. Ross
1959, Professional Paper 296
This report summarizes available data on two adjacent and partly overlapping regions in northwestern Montana. The first of these is Glacier National Park plus small areas east and west of the park. The second is here called, for convenience, the Flathead region; it embraces the mountains from the southern tip...
Allen V. Heyl Jr., Allen F. Agnew, Erwin J. Lyons, Charles H. Behre Jr., Arthur E. Flint
1959, Professional Paper 309
The upper Mississippi Valley zinc-lead district includes the southwest part of Wisconsin, the northwest corner of Illinois, and a narrow fringe of Iowa extending from Bellevue to McGregor, just west of the Mississippi River. The total area of the district is 4,000 square miles. The entire district is drained by...
W. W. Patton Jr., J.J. Matzko
1959, Professional Paper 302-A
Ralph Hile, Howard J. Buettner
1959, Research Report 51
No abstract available....