E P Laine
Biographic Data
| ID | 11137214 |
|---|---|
| NAME | E P Laine |
| GIVEN NAMES | E P |
| FAMILY NAME | Laine |
| SIGNATURE | LAINE E P |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 1984 |
| LATEST PUBLICATION YEAR | 1985 |
| H-INDEX | 0 |
Erosion of the Laurentide Region of North America by Glacial and Glaciofluvial Processes
Collection of seismic reflection data from continental margins and ocean basins surrounding North America makes it possible to estimate the amount of material eroded from the area formerly covered by Laurentide ice sheets since major glaciation began in North America. A minimum estimate is made of 1.62 × 10 6 km 3 , or an average 120 m of rock physically eroded from the Laurentide region. This figure is an order of magnitude higher than earlier e…
High Resolution Isotope Study of the Latest Deglaciation Based on Bermuda Rise Cores
A stable isotope and 14 C investigation of carbonates from three late Quaternary cores with high rates of sedimentation from the northeastern Bermuda Rise has produced the highest resolution record of the glacial maximum to Holocene stable isotope change yet obtained from an open ocean location. The record includes a three-step “termination” and the first direct evidence of an early deglacial meltwater “spike” in the open sea.
No prominent works on this page.
High Resolution Isotope Study of the Latest Deglaciation Based on Bermuda Rise Cores
A stable isotope and 14 C investigation of carbonates from three late Quaternary cores with high rates of sedimentation from the northeastern Bermuda Rise has produced the highest resolution record of the glacial maximum to Holocene stable isotope change yet obtained from an open ocean location. The record includes a three-step “termination” and the first direct evidence of an early deglacial meltwater “spike” in the open sea.
Erosion of the Laurentide Region of North America by Glacial and Glaciofluvial Processes
Collection of seismic reflection data from continental margins and ocean basins surrounding North America makes it possible to estimate the amount of material eroded from the area formerly covered by Laurentide ice sheets since major glaciation began in North America. A minimum estimate is made of 1.62 × 10 6 km 3 , or an average 120 m of rock physically eroded from the Laurentide region. This figure is an order of magnitude higher than earlier e…
Deglaciation (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Glacial period (2 works) · Meltwater (2 works) · Oceanography (2 works) · Paleontology (2 works) · Paleontology and Stratigraphy of Fossils (2 works) · Sediment (2 works) · Cryosphere (1 work)