Michael S. Marlow, A. K. Cooper, D.W. Scholl, T. R. Alpha
1976, Open-File Report 76-652
No abstract available....
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Page 5394, results 134826 - 134850
Publication Extents
Not all publications have extents, not all extents are completely accurateDonald A. Swanson, Wendell A. Duffield, Richard S. Fiske
1976, Professional Paper 963
Kathleen M. Blean
1976, Open-File Report 76-654
No abstract available. ...
Maurice A. Chaffee, J. Lee-Moreno, L.F. Caire, E. L. Mosier, J. G. Frisken
1976, Open-File Report 76-559
Michael L. Batzle, Stephen E. Hammond, Karen R. Christopherson
1976, Open-File Report 76-701-C
Edwin H. McKee
1976, Professional Paper 931
Philip Burke King
1976, Professional Paper 902
Philip Burke King, Helen Marie Beikman
1976, Professional Paper 903
Michael L. Batzle, Stephen E. Hammond, Vladimir Farkash
1976, Open-File Report 76-701-B
Harald D. Drewes
1976, Professional Paper 915
Michael L. Batzle, Stephen E. Hammond, Vladimir Farkash
1976, Open-File Report 76-701-A
No abstract available....
Sidney R. Ash, Charles Brian Read, R.A. Zeller Jr.
1976, Professional Paper 874
No abstract available....
J.H. Sass, H.A. Wollenberg, D. E. di Somma, J.P. Ziagos
1976, Open-File Report 76-862
Durl Edward Burkham
1976, Professional Paper 655-J
No abstract available....
Michael L. Batzle, Stephen E. Hammond, Karen R. Christopherson
1976, Open-File Report 76-701-D
R.L. Hanson, D.R. Dawdy
1976, Professional Paper 655-L
Durl Edward Burkham
1976, Professional Paper 655-I
J. Thomas Nash
1976, Professional Paper 907-D
Fluid-inclusion studies of 37 porphyry copper deposits, mainly in the United States, demonstrate that all but 3 evolved through a hydrothermal stage characterized by very high salinities, generally in excess of about 35 weight percent NaCI equivalent. Temperatures of these fluids ranged from about 250 deg to 700 deg C...
George C. Taylor Jr.
1976, Professional Paper 911
The review describes the history of the U.S. Geological Survey 's (USGS) activities in international water-resources investigations and institutional development as well as exchange in scientific and applied hydrology during 1940-70. The bulk of these activities has been carried out under the auspices of the U.S. Department of State, U.S....
Daniel R. Shawe
1976, Professional Paper 576-E
William W. Dudley Jr., J. D. Larson
1976, Professional Paper 927
The Ash Meadows area, at the southern tip of the Amargosa Desert in southern Nevada, discharges ground water collected over several thousand square miles of a regional flow system developed in Paleozoic carbonate rocks. Water moves westward across fault contacts from the bedrock into poorly interconnected gravel, sand, and terrestrial-limestone...
Daniel R. Shawe
1976, Professional Paper 576-D
William Albert Oliver Jr.
1976, Professional Paper 869
Elizabeth B. Tourtelot, James David Vine
1976, Professional Paper 907-C
Copper deposits occur in sedimentary and volcanogenic rocks within a wide variety of geologic environments where there may be little or no evidence of hydrothermal alteration. Some deposits may be hypogene and have a deep-seated source for the ore fluids, but because of rapid cooling and dilution during syngenetic deposition...
Joseph M. Boyce, Arthur L. Dial, Harold Masursky
1976, Open-File Report 76-624