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pro vyhledávání: '"Richard F. Sanford"'
Autor:
Richard F. Sanford
Publikováno v:
Economic Geology. 89:341-360
Tabular sandstone uranium deposits constitute the largest uranium resource type in the United States. A major point of contention has been the nature and direction of the ground-water flow. This paper presents a quantitative simulation of regional gr
Publikováno v:
Mathematical Geology. 25:59-80
Geochemical data are commonly censored, that is, concentrations for some samples are reported as “less than” or “greater than” some value. Censored data hampers statistical analysis because certain computational techniques used in statistical
Autor:
Richard F. Sanford
Publikováno v:
Economic Geology. 87:2041-2055
Tabular-type uranium deposits occur as tabular, originally subhorizontal bodies entirely within reduced fluvial sandstones of Late Silurian age or younger. This paper proposes that belts of tabular-type uranium deposits formed in areas of mixed local
Autor:
Richard F. Sanford
Publikováno v:
Geological Society of America Bulletin. 104:1236-1245
The Uncompahgre caldera, and the Lake City caldera nested within it, each have fossil hydrothermal systems and associated mineral deposits that formed during multiple episodes of mineralization during Oligocene and Miocene time. New lead isotopic ana
Autor:
Richard F. Sanford
Publikováno v:
Geology. 18:1099
Hydrogeologic modeling shows that tabular-type uranium deposits in the grants uranium region of the San Juan basin, New Mexico, formed in zones of ascending and discharging regional ground-water flow. The association of either lacustrine mudstone or
Autor:
Richard F. Sanford
Publikováno v:
Computers & Geosciences. 8:235-263
Geological examples of binary diffusion are numerous. They are potential indicators of the duration and rates of geological processes. Analytical solutions to the diffusion equations generally do not allow for variable diffusion coefficients, changin
Autor:
Richard F. Sanford
Publikováno v:
American Journal of Science. 282:543-616
The Redcloud Peak and Handies Peak Wilderness Study Areas are located 2-12 mi southwest of Lake City, CO. Much of the study areas has high mineral resource potential for precious and base metals in various ore deposit types. The rest of the study are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f5fec5661a1af491546e09eb38d034d
https://doi.org/10.3133/b1715b
https://doi.org/10.3133/b1715b
Publikováno v:
Open-File Report.
The Little Wood River Wilderness Study Area is in south-central Idaho 12 mi west-northwest of Hailey. This study area consists of Paleozoic sedimentary rocks overlain by Tertiary volcanic rocks. The parts of this study area that are underlain by Pale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eea4305a59ce4a895674fe902d2b169f
https://doi.org/10.3133/b1721d
https://doi.org/10.3133/b1721d