Norman J. Silberling
1959, Professional Paper 322
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateDorothy B. Vitaliano, S.T. Vesselowksy, and others
1959, Bulletin 1106-B
E.B. Eckel, Charles Milton, P.T. Sulsona
1959, Professional Paper 327
James Alfred Calkins, R. L. Parker, Alan Eastman Disbrow
1959, Open-File Report 59-15
No abstract available....
Darwin L. Rossman
1959, Bulletin 1058-B
Russell H. Brown
1959, Open-File Report 59-12
Russell H. Brown
1959, Open-File Report 59-14
R. M. Garrels (compiler), E.S. Larsen
1959, Professional Paper 320
Martha S. Carr, Carl E. Dutton
1959, Bulletin 1082-C
The importance of iron ore, the basic raw material of steel, as a fundamental mineral, resource is shown by the fact that about 100 million long tons of steel is used annually in the economy of the United States, as compared with a combined total of about 5 million long...
R. W. Imlay
1959, Professional Paper 314-G
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...
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...
C. A. Kaye, Z. S. Altschuler
1959, Professional Paper 317-C
No abstract available....
A.H. Lachenbruch
1959, Bulletin 1083-A
P.E. Byerly, H.R. Joesting
1959, Professional Paper 316-C
No abstract available....
C. A. Kaye
1959, Professional Paper 317-B
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...
Lee Carlton Dutcher, W.L. Burnham
1959, Open-File Report 59-38
Frederick Northrup Houser, Forrest Graham Poole
1959, Trace Elements Memorandum 1031
The Marble exploration hole 3 is in the northern part of the Tippipah Spring NE 7-1/2 minute quadrangle at the north end of Yucca Valley (fig.1). The collar elevation of the hole is about 5,316 feet and has the approximate Nevada State coordinates of N. 903,093 and E. 674,870. The...
Alfred T. Miesch
1959, Trace Elements Investigations 511
Norman M. Denson, G. O. Bachman, James R. Gill, William J. Hail Jr., Roy C. Kepferle, William J. Mapel, Harold Masursky, Robert E. Melin, George W. Moore, George N. Pipiringos, Charles B. Read, James M. Schopf, James D. Vine, Howard D. Zeller
1959, Bulletin 1055
No abstract available....
J. F. Poland, Allen Sinnott
1959, Water Supply Paper 1471
No abstract available....
Verl Richard Wilmarth
1959, Trace Elements Investigations 756
Francis Alexander McKeown, Verl Richard Wilmarth
1959, Trace Elements Memorandum 1036
The Marble exploration hole 4 was drilled to determine the chemical and physical properties of marble from the surface to depth of about 1,200 feet. The drill hole is in the north-central part of the Tippipah Spring quadrangle, approximately 40 miles north of Mercury, Nev. The collar of the hole...