Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Walter S. White"'
Autor:
Walter S. White
Publikováno v:
The Earth Beneath the Continents
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a1478899365d92013506a67199edd4fe
https://doi.org/10.1029/gm010p0028
https://doi.org/10.1029/gm010p0028
Autor:
Richard H. Jahns, Walter S. White
Publikováno v:
The Journal of Geology. 58:179-220
The formations of central and east-central Vermont are exposed as a series of parallel belts that strike nearly north. Most of the rocks dip steeply, and many are overturned. With one possible exception, there seem to be no major repetitions within t
Autor:
James C. Wright, Walter S. White
Publikováno v:
Economic Geology. 61:1171-1190
Pyrite is the characteristic sulfide mineral throughout most of the Nonesuch Shale, which is 400 to 600 feet thick. In a zone 1 to 50 feet thick at the base of the formation, the dominant sulfide is chalcocite. The top of this cupriferous zone is mar
Autor:
Walter S. White
Publikováno v:
The Journal of Geology. 67:577-581
1956b, Micropaleontological and isotopic determinations of Pleistocene climates: Micropaleontology, v. 2, no. 3, p. 257-270. SUESS, H. E., 1956, Absolute chronology of the last glaciation: Science, v. 123, p. 355-357. WISEMAN, J. D. H., 1954, The det
Autor:
Walter S. White
Publikováno v:
Economic Geology. 66:1-13
Pertinent physical properties of the upper Keweenawan rocks can be measured or inferred within a sufficiently narrow range to make the quantitative evaluation of various paleohydrologic models for the origin of the White Pine copper deposit feasible.
Autor:
Walter S. White
Publikováno v:
Circular.
Publikováno v:
Open-File Report.
Publikováno v:
Open-File Report.
Autor:
N.M. Denson, Walter S. White
Publikováno v:
Circular.