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Publication Extents

Not all publications have extents, not all extents are completely accurate
Volcanism in the western San Juan Mountains, Colorado
R. G. Luedke, W. S. Burbank
1966, Bulletin Volcanologique (29) 345-346
Three major cycles of volcanism during the Miocene and Pliocene formed a layered succession of calc-alkaline eruptive materials in the western San Juan Mountains nearly 1.5 miles thick and having a volume greater than 1,000 cubic miles. Each cycle was characterised by major eruptions followed by subsidence in the vent areas, and the resulting structure was a great volcanic plateau surrounding...
Crustal study of a continental strip from the Atlantic Ocean to the Rocky Mountains
I. Zietz, Elizabeth R. King, Wilburt Geddes, E.G. Lidiak
1966, Geological Society of America Bulletin (77) 1427-1447
Twenty aeromagnetic profiles over a 100-mile-wide strip along the arc of a great circle passing through Denver, Colorado, and Washington, D. C, reveal large anomalies of major crustal significance. Contoured data disclose several areas of distinct magnetic patterns reflecting basement lithology and structure. The mafic rocks of the Blue Ridge and Piedmont and the Keweenawan mafic belt in...
Magnetic data on the structure of the central Arctic Region
E. R. King, I. Zietz, L.R. Alldredge
1966, Geological Society of America Bulletin (77) 619-646
A study of 23,000 miles of total intensity aeromagnetic profiles in the central Arctic has been made by the U. S. Geological Survey and the U. S. Coast and Geodetic Survey. The profiles were flown at 20,000 feet above sea level and cover approximately 1,350,000 square miles of the Arctic Ocean between the North Pole...
Geochronology of the St. Kevin granite and neighboring precambrian rocks, northern Sawatch Range, Colorado
R. C. Pearson, C. E. Hedge, H.H. Thomas, T.W. Stern
1966, Geological Society of America Bulletin (77) 1109-1120
Radiometric ages have been measured on rocks of a crystalline terrane that includes ancient gneisses and migmatites, two granitic batholiths (St. Kevin Granite and granite of Cross Creek), and various minor intrusive rocks. A whole-rock Rb-Sr isochron age on the St. Kevin Granite establishes it as 1390 ± 60 m.y. old. Mineral ages on the St. Kevin and numerous other rocks are either about the same as the St. Kevin whole-rock age...
Large-scale basin-and-dome pattern resulting from the interference of major folds
O. T. Tobisch
1966, Geological Society of America Bulletin (77) 393-408
The geometry of individual major folds from the Glen Cannich area in the Northern Highlands of Scotland is described. The major folds are isoclinal, and their axial planes and fold limbs strike north or northeast and dip steeply; the fold axes plunge steeply toward the south or southeast. If pairs of individual folds are joined along a common axial-plane trace they form basins, domes, or other unusual...
Eclogitic pyroxenes, ordered with P2 symmetry
J. R. Clark, J. J. Papike
1966, Science (154) 1003-1004
X-ray diffraction crystal-structure analysis of omphacite from eclogite, Tiburon Peninsula, Marin County, California, shows that this clinopyroxene has P2 symmetry with a nearly ordered distribution of the multiple cation content defined by its approximate formula: (Na0.5Ca0.5) (Mg0.4Fe2+0.1Al0.4Fe3+0.1)Si2O6. Na+ and Ca2+ tend to assume alternate locations in the structure, and...
Absence of neutral alkali atoms in rhodizite
G. Donnay, A. N. Thorpe, F. E. Senftle, R. Sioda
1966, Science (154) 889-890
The formula CsB12Be4Al4O28 has been proposed by others for the mineral rhodizite. Electron-spin-resonance and magnetic susceptibility measurements prove the absence of neutral cesium atoms. An ionic formula CsB11Be4Al4O26(OH)2 is proposed....
Nickel-iron spherules from Aouelloul glass
E. C. T. Chao, E.J. Dwornik, C.W. Merrill
1966, Science (154) 759-765
Nickel-iron spherules, ranging from less than 0.2 to 50 microns in diameter and containing 1.7 to 9.0 percent Ni by weight, occur in glass associated with the Aouelloul crater. They occur in discrete bands of siliceous glass enriched in dissolved iron. Their discovery is significant tangible evidence that both crater...
Sulfide-mineral zoning in the basal nonesuch shale, Northern Michigan
W. S. White, J.C. Wright
1966, Economic Geology (61) 171-1190
A zone, 1 to 50 feet thick, at the base of the Nonesuch Shale, is relatively rich in copper, chiefly as chalcocite. Pyrite is the characteristic sulfide mineral of the overlying 400 to 600 feet of the formation. The boundary of the cupriferous zone with the pyrite zone regionally transgresses both stratigraphic layering and fades gradations indicative...
Observations on the Life History of Ogcodes rufoabdominalis in Northern Utah (Diptera: Acroceridae)
K.J. Capelle
1966, Journal of the Kansas Entomological Society (39) 641-649
Detailed observations were made on the emergence and feeding habits of the acrocerid parasite Ogcodes rufoabdominalis from lycosid spiders. One hundred and twenty field-collected hosts yielded six parasites in May. Eggs, first and third instars, and pupae are described for the first time, as well as mating and oviposition....
Proportion of recovered goose and brant bands that are reported
R. K. Martinson, J.A. McCann
1966, Journal of Wildlife Management (30) 856-858
A few more than one-third of the goose and brant bands recovered by hunters were reported to the Bird Banding Laboratory (a rate of 0.361) during the 1962-64 hunting seasons. We calculated this band-reporting rate by comparing the estimated number of goose and brant bands recovered by hunters, based on...
Flexible plastic collars compared to nasal discs for marking geese
G.A. Sherwood
1966, Journal of Wildlife Management (30) 853-855
Construction of a flexible plastic collar for marking geese is described. The usefulness of the collars, tried on 468 Canada geese (Branta canadensis) at the Seney National Wildlife Refuge from 1963 to 1965, was compared with that of nasal discs attached to 361 Canada geese at Seney in 1961 and...
Breeding ecology of the redhead duck in western Montana
J. T. Lokemoen
1966, Journal of Wildlife Management (30) 668-681
The habits of the redhead duck (Aythya americana) were studied in the Flathead Valley of western Montana in 1960 and 1961 to determine their habitat preferences in this pothole breeding ground. The 2,600-acre study area, surrounding the Ninepipe Reservoir, contained 686 potholes. Redheads usually were paired by the time they...
Use of analog model to predict streamflow depletion, big and little Blue River basin, Nebraska
P. A. Emery
1966, Groundwater (4) 13-19
The States of Nebraska and Kansas are negotiating a compact for apportionment of the waters of the Big and Little Blue Rivers. So that the negotiating officials could allocate the water equitably, the amount of streamflow depletion caused by ground‐water withdrawals upgradient from the State line needed to be determined. At the request of the Nebraska officials, the U. S. Geological Survey...
Frequency distribution of dissolved solids in ground water
G.H. Davis
1966, Groundwater (4) 5-12
The frequency distribution of dissolved‐solids content of ground waters in geologically and climatologically homogeneous terrane units commonly approximates a log‐normal distribution. A graphic logarithmic transformation is de‐scribed which permits rapid calculation of approximate values for the mean, standard deviation, and coefficient of variation. Statistical parameters calculated by this method show good agreement with known physical conditions in the terranes studied and are...
The effect of climate on drainage density and streamflow
C.W. Carlston
1966, International Association of Scientific Hydrology - Bulletin (11) 62-69
Sir Charles Cotton (1964) has pointed out that in an earlier paper (Carlston, 1963) which related drainage density to hydrology, there was insufficient emphasis on the role of climate in its effect on drainage density. Re-examination of the relation of drainage density to base flow in the 15 basins originally...
Calcium and bromide contents of natural waters
R.J. Anderson, D. L. Graf, B.F. Jones
1966, Science (153) 1637-1638
The linear relation observed in a log Ca++ versus log Br- plot for subsurface Cl- waters is attributed to ultrafiltration by shale of sea water and fresh water that have passed through sedimentary rocks since their formation. Reactions between these solutions and sedimentary minerals, particularly dolomitization, must have contributed additional Ca++ to solution....
Airborne geophysical study in the Pensacola Mountains of Antarctica
John C. Behrendt, L. Meister, J. R. Henderson
1966, Science (153) 1373-1376
A seismic reflection, gravity, and aeromagnetic reconnaissance was made in the Pensacola Mountains, Antarctica, during the 1965-66 austral summer. Prominent ice streams located between the Neptune and Patuxent Ranges and east of the Forrestal Range overlie...
Genetic relations of oceanic basalts as indicated by lead isotopes
M. Tatsumoto
1966, Science (153) 1094-1101
The isotopic compositions of lead and the concentrations of lead, uranium, and thorium in samples of oceanic tholeiite and alkali suites are determined, and the genetic relations of the oceanic basalts are discussed. Lead of the oceanic tholeiites has a varying lead-206 : lead-204 ratio between 17.8 and 18.8, while...
Oxygen fugacities directly measured in magmatic gases
M. Sato, T. L. Wright
1966, Science (153) 1103-1105
An electrochemical device was used to measure the fugacity of oxygen (fO2) in holes drilled through the crust of Makaopuhi lava lake, Kilauea Volcano, Hawaii. Results obtained within 6 months of the lake formation show that log fO2 normally varies linearly with the reciprocal of the absolute temperature, and that chemical changes...