G Vilks
Biographic Data
| ID | 6371428 |
|---|---|
| NAME | G Vilks |
| GIVEN NAMES | G |
| FAMILY NAME | Vilks |
| SIGNATURE | VILKS G |
| AFFILIATIONS | Geological Survey of Canada |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 3 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1970 |
| LATEST PUBLICATION YEAR | 1989 |
| H-INDEX | 0 |
Evidence for Wisconsinan Glaciations in the Verrill Canyon Area, Scotian Slope
A composite thickness of about 25 m of sediment has been cored from the Verrill Canyon on the Scotian Slope. It is interpreted that the majority of this sequence was deposited in a glaciomarine environment during oxygen isotopic stage 2 and the top of stage 3. These sediments, as seen in high-resolution seismic reflection profiles, are well stratified, become thicker upslope, are laterally variable in thickness, and pass upslope into possible out…
Marine Geological Program in the Byam Martin ChannelLougheed Island Region, District of Franklin
Circulation of Surface Waters in Parts of the Canadian Arctic Archipelago Based on Foraminiferal Evidence
The distribution of planktonic foraminifera, collected 27 May-15 July 1968 from sea ice in McClure Strait, indicates a slow net eastward movement of water from the Arctic Ocean through the strait in the past with increased rates at present. The bottom topography, regional climatology and oceanography of the area are discussed
No prominent works on this page.
Circulation of Surface Waters in Parts of the Canadian Arctic Archipelago Based on Foraminiferal Evidence
The distribution of planktonic foraminifera, collected 27 May-15 July 1968 from sea ice in McClure Strait, indicates a slow net eastward movement of water from the Arctic Ocean through the strait in the past with increased rates at present. The bottom topography, regional climatology and oceanography of the area are discussed
Marine Geological Program in the Byam Martin ChannelLougheed Island Region, District of Franklin
Evidence for Wisconsinan Glaciations in the Verrill Canyon Area, Scotian Slope
A composite thickness of about 25 m of sediment has been cored from the Verrill Canyon on the Scotian Slope. It is interpreted that the majority of this sequence was deposited in a glaciomarine environment during oxygen isotopic stage 2 and the top of stage 3. These sediments, as seen in high-resolution seismic reflection profiles, are well stratified, become thicker upslope, are laterally variable in thickness, and pass upslope into possible out…
Geology (2 works) · Geology (2 works) · Oceanography (2 works) · Oceanography (2 works) · Archaeology (1 work) · Archaeology and Natural History (1 work) · Archipelago (1 work) · Arctic (1 work) · Arctic ice pack (1 work) · Benthic zone (1 work)