Zobrazeno 1 - 10
of 48
pro vyhledávání: '"L H Thorleifson"'
Publikováno v:
Aquatic Ecosystem Health & Management. 9:307-318
Lake Winnipeg supports the largest commercial fishery on Canadian Prairies. It has been influenced by a variety of environmental forces and anthropogenic activities. To gain a better understanding of recent changes in nutrient status of the lake, it
Publikováno v:
Ore Geology Reviews. 16:145-166
This paper summarizes advances since 1987 in the application of glacial sediment sampling to mineral exploration (drift prospecting) in areas affected by continental or alpine glaciation. In these exploration programs, clastic glacial sediments are t
Publikováno v:
Journal of Paleolimnology. 19:365-376
Estimates of postglacial rebound in central North America from Laurentide deglaciation to the present time are uncertain as a result of lack of data from the continental interior. A more precise knowledge of postglacial tilt history will assist studi
Publikováno v:
Journal of Paleolimnology. 19:215-243
Lake Winnipeg, the seventh largest lake in North America, is located at the boundary between the Interior Plains and the Canadian Shield in Manitoba, Canada. Seismic profiles were obtained in Lake Winnipeg on two geoscientific cruises in 1994 and 199
Autor:
L. H. Thorleifson
Mineral exploration methods ranging from boulder tracing to elemental and indicator mineral methods utilize clastic debris transported from mineralized bedrock sources. An understanding of glacial process and history, combined with sound survey desig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::792e081513cf33a991bd943fd8d15b85
https://doi.org/10.4095/292681
https://doi.org/10.4095/292681
Autor:
Michel Lamothe, Banks Miller, Glenn W. Berger, J.-S. Vincent, Peter U. Clark, J.P. Szabo, John J. Clague, R.R. Stea, Nicholas Eyles, Gifford H. Miller, R.N. Oldale, L. H. Thorleifson, Stephen R. Hicock, B. Brandon Curry, Aleksis Dreimanis, Robert J. Mott
Publikováno v:
Quaternary Science Reviews. 12:79-114
Fossil records from sites overridden by or adjacent to the Laurentide Ice Sheet indicate that the climate of the last interglaciation (Oxygen-Isotope Substage 5e, ca. 130-116 ka) was warmer than today. Following the last interglaciation, the Laurenti