Zobrazeno 1 - 10
of 46
pro vyhledávání: '"Robert H. Osborne"'
Sources of beach sand at creciente island, Baja California Sur, Mexico: Fourier grain-shape analysis
Publikováno v:
Ciencias Marinas. 20:243-266
Fourier grain-shape analysis (FGSA) of detrital quartz grain was used to identify local sources for medium-grained (0.25 to 0.50 mm) sand in Creciente barrier island, which is located on the west coast of Baja California Sur, Mexico. A total of 52 sa
Autor:
Melinda L. Marian, Robert H. Osborne
Publikováno v:
Canadian Journal of Earth Sciences. 29:2595-2609
The Beck Spring Dolomite is the medial unit of the Middle to Late Proterozoic Pahrump Group, the oldest sequence of sedimentary rocks in eastern California. Stratigraphic sections of the Beck Spring Dolomite examined in the eastern Mojave Desert and
Autor:
Robert H. Osborne, Randall L. Moory
Publikováno v:
Environmental & Engineering Geoscience. :355-369
Balboa Island was created from 1929 to 1935 by filling a sand shoal with dredge spoil from associated channels and berth areas in Lower Newport Bay. This east-trending island is approximately 1,160 m long and 460 m wide, and is protected by concrete
Publikováno v:
SEPM Journal of Sedimentary Research.
Autor:
Robert H. Osborne
From Shoreline to Abyss: Contributions in Marine Geology in Honor of Francis Parker Shepard - Francis P. Shepard left a rich scientific legacy including more than 230 published papers and books primarily addressed to the study of submarine canyons an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13b2b915cb37b4545a83882a052a8c33
https://doi.org/10.2110/pec.91.09
https://doi.org/10.2110/pec.91.09
Publikováno v:
Sedimentology. 23:689-703
During the period from 1967 through 1972, a sampling programme was completed to determine the economic potential of heavy metals in the beach and river sands of the southern California coastal zone. These samples were employed to test the hypothesis
Publikováno v:
Tectonophysics. 98:209-251
The San Gabriel fault, a deeply eroded late Oligocene to middle Pliocene precursor to the San Andreas, was chosen for petrologic study to provide information regarding intrafault material representative of deeper crustal levels. Cataclastic rocks exp